Report on the 2014 Phase 3 Diamond Drilling Program: Sunday Lake Project

Report on the 2014 Phase 3 Diamond Drilling Program: Sunday Lake Project Transition Metals Corp. and Impala Platinum Holdings Limited Written By: September 7 th, 2016 Steven Flank Project Geologist Grant Mourre Exploration Manager

Contents Introduction... 3 Location... 3 Land Tenure... 3 Regional Geology... 6 Local Geology... 7 Geology of the Sunday Lake Intrusion... 8 Previous Work... 9 Diamond Drilling... 10 Summary Logs... 11 Summary... 11 Conclusions... 13 Signatures... 15 Appendix A: Diamond Drill Logs... 16 Appendix B: Drill Plan and Cross Sections... 17 Appendix C: Assays... 18 Figure 1: Sunday Lake Project Location Map... 4 Figure 2: Sunday Lake Land Tenure with claim numbers.... 5 Figure 3: Geology of the Midcontinent Rift with notable mineral deposits and intrusions.... 6 Figure 4: Surficial geology of the Sunday Lake Property. Approximate plan extent of intrusion shown as brown dashed line... 8 Figure 5: Plan map of drilling to date (top, reduced to pole total magnetic intensity image shown) and conceptual cross-section (bottom)... 12 Table 1: Sunday Lake claim details... 3 Table 2: 2014 Phase 3 Diamond Drill Holes... 10 Table 3: Significant Intersections from the 2014 Phase 3 diamond drilling program... 10 Table 4: Significant intersections on the Sunday Lake Property... 13

Introduction The Sunday Lake Project is a PGM-Cu-Ni exploration project located 25km north of Thunder Bay Ontario within the Midcontinent Rift (MCR). The project is managed under a joint venture agreement between Impala Platinum (Implats) and Transition Metals Corp. (TMC). In January 2014 TMC reported results from a Phase 1 diamond drilling program which identified high grade, platinum rich, PGM(Pt+Pd+Au)- Cu-Ni mineralization within the Sunday Lake Intrusion (SLI). Following this discovery, exploration programs including borehole electromagnetic surveys, ground magnetic and ground gravity surveys, geologic mapping and a 5 hole 2,550m diamond drilling program were completed in the spring and summer of 2014. This report documents the results of the Phase 3 diamond drilling program completed between November 7 th, 2014 and January 23 rd, 2015. Location The Sunday Lake Project is located approximately 25km north of the City of Thunder Bay, Ontario. It is comprised of staked mining claims, optioned mining claims, optioned patents and leased patents which cover 2612ha (Figure 1). Access to the Sunday Lake property is attained by travelling north on Hwy. 527 from Thunder Bay, Ontario for 25km to Barnum Lake road. Travel west on Barnum Lake road for 7.5km to an unmarked, unmaintained logging road known as Ton Lake Road. The Ton Lake Road is followed west for another 7.5km to access the property. Land Tenure The Sunday Lake property is comprised of 11 claims totalling 98 units and 6 privately owned patents (19888, 19889, 19890, 10083, 6041, 6056). Claim information is summarized in Table 1 and illustrated in Figure 2. Table 1: Sunday Lake claim details Township / Area Claim Number Recording Date Claim Due Date Work Required Total Applied Total Reserve JACQUES 4210856 2006-Aug-18 2018-Aug-18 $3,200 $32,000 $0 JACQUES 4210857 2006-Aug-18 2018-Aug-18 $2,400 $24,000 $0 JACQUES 4210858 2006-Aug-18 2018-Aug-18 $4,000 $40,000 $52,361 JACQUES 4230099 2008-Feb-21 2018-Feb-21 $4,800 $38,400 $0 JACQUES 4247181 2010-Oct-18 2018-Oct-18 $800 $4,800 $25,058 JACQUES 4274640 2013-May-13 2018-May-13 $4,000 $12,000 $0 JACQUES 4276395 2013-Nov-04 2018-Nov-04 $4,800 $14,400 $0 JACQUES 4282597 2016-Feb-19 2018-Feb-19 $3,200 $0 $0 JACQUES 4282598 2016-Feb-19 2018-Feb-19 $1,200 $0 $0 ONION LAKE AREA 3009143 2005-Feb-11 2018-Feb-11 $3,200 $35,200 $98,854 ONION LAKE AREA 4210859 2006-Aug-18 2018-Aug-18 $4,800 $48,000 $212,818 ONION LAKE AREA 4210860 2006-Aug-18 2018-Aug-18 $3,200 $32,000 $13,397 ONION LAKE AREA 4210861 2006-Aug-18 2018-Aug-18 $3,200 $32,000 $7,310 ONION LAKE 4274641 2013-May-13 2018-May-13 $5,600 $16,800 $0

AREA ONION LAKE AREA ONION LAKE AREA 4276394 2013-Nov-04 2018-Nov-04 $6,000 $18,000 $0 4276396 2013-Nov-04 2017-Nov-04 $2,735 $14,065 $0 Figure 1: Sunday Lake Project Location Map

Figure 2: Sunday Lake Land Tenure with claim numbers.

Regional Geology The Sunday Lake Intrusion is a Proterozoic aged mafic-ultramafic intrusion associated with the ~1.1 Ga MCR. The MCR is believed to be an ancient failed rift which is expressed as a 2,500km long arcuate shaped package of volcanic, sedimentary and intrusive which extends from Kansas, through Lake Superior and terminating at the Grenville front in Northern Michigan (Figure 3). Exploration of MCR related intrusions has persisted for decades within the Duluth Complex, the Great Lakes Nickel Deposit and the Coldwell Complex (Marathon deposit) focusing largely on the base metal potential of these large tonnage, low grade deposits. As the geological understanding of the MCR became better understood, researchers recognized the potential for world class Ni-Cu-PGM deposits similar to those hosted in the analogous Norilsk mining camp of Russia. This information, coupled with rising precious metal prices in the late 1990 s early 2000 s spurred a flurry of exploration activity in the region. This activity ultimately led to new discoveries in Michigan (Eagle Mine), Minnesota (Tamarack deposit) and in Ontario (Thunder Bay North Deposit). Unlike the large tonnage, low grade deposits previously discovered, these new discoveries boasted high grade Ni-Cu dominated mineralization at Eagle and Tamarack, and high grade PGM dominated mineralization at Thunder Bay North. Mineralization is hosted within irregularly shaped, primitive, ultramafic to mafic intrusions associated with the earliest stages of rift development. As such it was recognized that these early-rift type intrusions were highly prospective for magmatic PGM-Cu-Ni mineralization. Figure 3: Geology of the Midcontinent Rift with notable mineral deposits and intrusions.

Local Geology The SLI is an early-rift type mafic-ultramafic intrusion that has intruded into metasedimentary and granitic rocks of the Quetico Subprovince. The main mass of the intrusion does not outcrop, with only a single ridge of diabasic gabbro found along the SW shore of Sunday Lake (Figure 4). Drilling has shown that the main body of the SLI is buried beneath up to 400m of Quetico metasediments. Towards the NW, where the intrusion transects the Archean granodiorite /metasediment contact, the hanging wall contact is shallower and was intersected at a depth of 61m in hole 12SL0002. Quetico Group sedimentary rocks dominate the southern portion of the property. These rocks are strongly foliated to gneissic with a strong E-W to NE-SW fabric and a steep dip. Gneissic textures are observed near the northern margin of the sediments, where a transitional contact with granodiorite is relatively well exposed. This transition zone occurs over a width of approximately 500m where bands and dykes of granodiorite and pegmatite truncate the sediments. Moving south from this contact, metamorphic grade and deformation weaken and relict bedforms (graded bedding/cross bedding) are observed in the turbiditic sediments. As the southernmost portion of the property is approached strong gneissic textures are again observed, possibly related to a contact with another Archean granite body (Barnum Lake stock) located south of the property. The granodiorite to the north is typically massive to weakly foliated, comprised of coarse grained plagioclase, alkali feldspar, biotite and minor quartz. Deformation is most intense proximal to the gneissic contact with the sediments to the south. Along this contact dykes or bands of granodiorite range from 1-5m in width and may be folded and boudinaged, making mapping of these units at depth difficult. The country rocks overlying the SLI show complex structure and alteration that appear to be the result of the emplacement and crystallization of the SLI. Wide zones of in-situ brecciation and localized fault breccia may represent pre-existing crustal scale structures that were utilized by the intrusion during it s ascent through the crust. A wide alteration halo, extending nearly 400m to surface in places, increases in intensity as the intrusion is approached suggesting it is derived from fluids generated by the SLI. Alteration grades from predominantly sericite and carbonate filled fractures to pervasive hematite alteration with chlorite and pyrite being confined to fractures. No PGM mineralization is associated with the pyritic breccias of the hanging wall. The footwall to the intrusion is typically bleached, with annealing textures that obscure the metamorphic fabric of the sediments. In-situ brecciation is common and appears more ductile rather than the brittle deformation that is observed in the hanging wall. Footwall mineralization consists of stringers and blebs of chalcopyrite that have exceptionally high PGM tenors (up to 5.06 g/t PGM from 608.4-609.1m in SL-13-006).

Figure 4: Surficial geology of the Sunday Lake Property. Approximate plan extent of intrusion shown as brown dashed line Geology of the Sunday Lake Intrusion The stratigraphy of the SLI based on the drilling to date can be broken down into three main units: Upper Gabbro Series (UGS), Lower Gabbroic Series (LGS) and Ultramafic Series. The UGS is an evolved, coarse grained plagioclase cumulate gabbro to monzogabbro which can be up to 348m thick. Rocks of the UGS are strongly hematite, epidote, chlorite and potassic altered. Thick sequences of gabbroic breccias are intermittently encountered at the upper contact of the intrusion and contain 10-50% angular quartz xenoliths within a strongly hemaitized gabbroic matrix. Upper Series rocks contain 1-5% disseminated pyrite but do not contain PGM mineralization. The LGS is in sharp contact with the UGS and is more mafic in character, comprised of gabbro to olivine melagabbronorite. The unit is distinct from the UGS, separated by a sharp contact, and is markedly finer grained. The LGS grades from and an upper gabbroic unit to a central melagabbo-peridotite before becoming more gabbroic again as the lower contact with the Ultramafic Series is approached. Minor PGM mineralization occurs at the interface between the UGS and LGS, with values not exceeding 1 g/t PGM.

The Ultramafic Series is the basal unit in the southern most drill holes and is comprised of olivine melagabbro, peridotite and minor pyroxenite. It is located beneath the LGS, separated by a sharp, variable textured contact possibly representing auto-brecciation of the overlying LGS. Its thickness ranges from approximately 10m in some drill holes near the north contact of the intrusion to 140m near the centre of the SLI. The Ultramafic Series is coarser grained and more strongly serpentinized than the LGS. Mineralization in the ultramafic series occurs within an olivine melagabbro unit with 2-10% disseminated, fine-grained cpy-py-po. Rare sulfide veins and semi-massive sulfide are also observed. Intersections of 20.2m @ 3.22 g/t PGM, 0.26% Cu and 0.11% Ni in SL-13-002 and 15m @ 2.84 g/t PGM, 0.22% Cu and 0.09% Ni in SL-14-003 are representative of the mineralization encountered in the Ultramafic Series. The size and shape of the intrusion is inferred from the available magnetic and gravity data and diamond drilling, indicates an elliptical body in plan view, elongated in along a NE-SW direction. The dimensions of the intrusion are inferred to be 1.3km wide and 2.9km long (Figure 4). Diamond drilling has shown that the upper contact of the SLI is located between 61m in the north and 424m in the south (average 350m). The lower contact of the intrusion ranges from 144m in the north to 1,153m in the south. The morphology of the SLI is inferred to be an elongated lopolith, with an axis that trends NE-SW deepening to the SW as indicated by drilling and gravity data. In the northern portion of the intrusion, a change in the lithology of the country rocks from metasedimentary to granodiorite correlates with a change in the morphology of the intrusion from a bowl-shaped body to an irregular dyke-sill or possibly a chonolith. Previous Work 2002: Probe Mines completes a MMI soil sampling program over a prominent magnetic feature outlined by a OGS regional magnetic survey 2006: Canstar Resources flies a 282 line km airborne magnetic survey over the Sunday Lake magnetic anomaly 2007: Canstar Resources completes a two hole, 484.4m diamond drilling program 2008: Magma Metals Canada Ltd. completes a single 735m drill hole which intersects gabbroic rocks of the Sunday Lake Intrusion. Borehole EM is completed on this hole. 2008: Kennecott Canada Exploration Inc. completes a 418.3 line km AeroTEM survey 2009: Kennecott Canada Exploration Inc. completes line cutting and a ground pulse EM survey 2010: Rio Tinto Exploration Canada Inc. completes a ground gravity survey 2011: Rio Tinto Exploration Canada Inc. extends the Magma Metals diamond drill hole for an additional 470m and intersects the basal contact of the Sunday Lake Intrusion. Borehole EM is completed on the entire hole.

2012: Rio Tinto Exploration Canada Inc. Rio Tinto Exploration Canada Inc. completes a one hole, 204m diamond drilling program with borehole EM. Anomalous PGM-Cu-Ni mineralization is encountered along the basal contact 2013: HTX Minerals completes line cutting, geological mapping and ground gravity, magnetic and surface pulse EM surveys. Work concludes with a six hole 2,544.3m diamond drilling program resulting in the discovery of significant PGM-Ni-Cu mineralization associated with the Sunday Lake intrusion (20.2m @ 3.22 g/t PGM, 0.26% Cu and 0.11% Ni in SL-13-002) 2014: Transition Metals Corp. completes a five hole 2,550m diamond drilling program with follow up borehole EM surveys. Highlights include 11.7m @ 2.79 g/t PGM, 0.37% Cu, 0.12% Ni and 15m @ 2.84 g/t PGM, 0.22% Cu and 0.09% Ni in SL-14-003) Diamond Drilling A total of 3 diamond drill holes totalling 2,074m were completed between November 7th, 2014 and January 18 th, 2014 which included a 19 day break from drilling between December 20 th and January 7 th. Orbit Garant Drilling of Val-d Or, Quebec was the sole drill contractor for this program. Drill hole location details are summarized in Table 2. Results of the diamond drilling program are summarized below with drill logs, plans and cross sections provided in Appendix A and B. A total of 420 samples were submitted for assay and of those samples 63 were analyzed for whole rock geochemistry. Assay highlights for the Phase 3 drill program are included in Table 3, with assay certificates in Appendix C. Table 2: 2014 Phase 3 Diamond Drill Holes DDH Easting Northing Azimuth Dip EOH SL-14-006 334833 5394962 270-85 863m SL-14-007 334332 5395250 295-75 497m SL-14-008 334332 5395250 290-85 714m Total 2,074m Drill Hole Table 3: Significant Intersections from the 2014 Phase 3 diamond drilling program From (m) To (m) Length (m) Pt (g/t) Pd (g/t) Au (g/t) PGM (Pt+Pd+Au) (g/t) Cu (%) Ni (%) SL-14-006 825.0 835.9 10.9 1.38 0.83 0.09 2.30 0.30 0.12 including 831.0 835.9 4.90 1.97 1.19 0.13 3.29 0.41 0.16 SL-14-008 656.6 674.4 17.8 1.17 0.7 0.08 1.95 0.27 0.11 including 656.6 663.6 7.00 1.99 1.19 0.12 3.30 0.37 0.15 including 661.6 662.6 1.00 4.03 2.37 0.20 6.60 0.65 0.22

Summary Logs SL-14-006 (863m: 270 /-85 ) 400m step out to the SE of intersections in SL-13-006, along the alteration trend outlined from geological mapping. The hole intersected 421.9m of the SLI from 414m. From 806.4-835.9m pyrrhotite and chalcopyrite mineralized ultramafic and gabbroic rock along above the basal contact were encountered, returning 10.9m of 2.3 g/t PGMs between 825-835.9m. Within this interval a higher grade zone returned values of 3.29g/t PGMs over 4.9m from 831-835.9m. SL-14-007 (497m: 295 /-75 ) 300m step out to the SW of SL-13-002 along the structural lineament that follows Sunday Lake. The hole intersected 90.6m of the SLI from 355.5-446.1m. No appreciable sulfide mineralization was encountered and no significant assays were returned. SL-14-008 (714m: 290 /-85 ) Planned as an infill hole to confirm the continuity of the mineralized zone between SL-13-006 and SL-14-006. The hole intersected 284.9m of the SLI from 393.9-678.8m. From 655.6-678.8m pyrrhotite and chalcopyrite mineralized ultramafic and gabbroic rocks along the basal contact were encountered returning 17.8m of 1.95 g/t PGM s. Within this interval a higher grade zone returned values of 3.28 g/t PGM s over 7.0m from 656.6-663.6m and 6.60 g/t PGM s over 1m from 661.6m. Summary The results of the Phase 3 diamond drilling program were very encouraging and helped provide valuable insight into the morphology of the SLI, as well as the mineralization distribution. Drilling and geophysical data suggest that the main mass of the intrusion measures approximately 2.9km x 1.3km and is a layered mafic/ultramafic lopolith, elongated along an NE-SW trending axis. The upper contact is relatively flat, dipping modestly to the south/south west, and is encountered at a depth of approximately 400m. The lower contact has a steeper dip, again to the south and west and is as deep as 1153.5m as demonstrated in historical hole 11SL0001. Table 4 summarizes significant intersections of mineralization on the Sunday Lake property. During the phase 3 drill program the mineralized zone was expanded to a strike length of 700m with the intersections in SL-14-006 and 008. Figure 5 shows a plan map and a cross section highlighting the distribution of mineralization encountered to date.

Figure 5: Plan map of drilling to date (top, reduced to pole total magnetic intensity image shown) and conceptual crosssection (bottom)

Table 4: Significant intersections on the Sunday Lake Property Drill Hole From (m) To (m) Length Pt Pd Au Pt+Pd+Au Cu Ni (m) (g/t) (g/t) (g/t) (g/t) (%) (%) S (%) SL-13-002 369.40 371.80 2.40 0.87 0.46 0.03 1.36 0.03 0.04 0.72 and 395.00 415.20 20.20 2.11 0.95 0.16 3.22 0.26 0.11 1.22 including 410.00 413.00 3.00 3.41 1.68 0.28 5.37 0.45 0.13 1.23 SL-13-003 299.00 308.00 9.00 0.91 0.74 0.08 1.73 0.44 0.13 3.05 including 302.00 303.00 1.00 1.73 1.43 0.15 3.31 0.86 0.24 3.05 SL-13-005 164.60 170.60 6.00 0.4 0.31 0.04 0.75 0.13 0.04 0.59 including 167.60 168.60 1.00 0.66 0.59 0.09 1.34 0.31 0.07 0.97 SL-13-006 567.00 575.00 8.00 1.23 0.72 0.09 2.04 0.20 0.08 0.48 and 595.70 602.40 6.70 0.87 0.68 0.05 1.60 0.32 0.17 2.36 including 602.00 602.40 0.40 3.94 3.82 0.06 7.82 1.98 1.10 18.30 and 602.40 612.10 9.70 0.75 0.49 0.06 1.30 0.21 0.04 0.95 including 607.40 609.10 1.70 2.84 1.74 0.25 4.83 0.77 0.05 1.11 SL-14-002 412.00 420.00 8.00 1.13 0.46 0.08 1.67 0.13 0.05 0.74 including 417.00 420.00 3.00 1.80 0.68 0.14 2.62 0.22 0.09 0.94 SL-14-003 389.30 401.00 11.70 1.79 0.94 0.06 2.79 0.12 0.04 2.49 including 391.00 396.00 5.00 3.25 1.65 0.10 5.00 0.14 0.04 3.67 including 393.00 394.00 1.00 6.34 3.22 0.19 9.75 0.24 0.06 3.37 and 501.50 502.10 0.60 0.82 0.68 0.06 1.56 0.24 0.11 0.90 and 526.00 541.00 15.00 1.8 0.92 0.12 2.84 0.22 0.09 0.58 including 532.00 540.00 8.00 2.52 1.16 0.17 3.85 0.30 0.10 0.75 SL-14-004 463.60 465.30 1.70 1.00 0.51 0.07 1.58 0.12 0.05 0.29 SL-14-005 512.00 516.80 4.80 0.61 0.39 0.04 1.04 0.18 0.09 1.23 SL-14-006 825.00 835.90 10.9 1.38 0.83 0.09 2.30 0.30 0.12 0.97 including 831.00 835.90 4.90 1.97 1.19 0.13 3.29 0.41 0.16 1.07 and (FW) 838.50 839.00 0.50 1.20 0.91 0.07 2.18 0.23 0.14 0.89 SL-14-008 656.60 674.40 17.80 1.17 0.70 0.08 1.95 0.27 0.11 NA including 656.60 663.60 7.00 1.99 1.19 0.12 3.30 0.37 0.15 NA Conclusions Significant PGM-Cu-Ni mineralization has been intersected in diamond drilling along the basal contact of the main mass of the SLI. Within the main mass, the morphology of the intrusion appears to be lopolithic, having a lateral extent of 2.9km x 1.3km. The entire basal contact across this 3.77km 2 area is considered to be prospective for additional accumulations of PGM-Cu-Ni mineralization and as such requires considerably more drilling to determine the resource potential of the SLI.

Exploration programs at Sunday Lake continue to expand on the geological understanding of this underexplored intrusion as well as expand the zone of PGM-Cu-Ni mineralization. The following conclusions can be drawn from the work completed to date: The SLI is an early-rift related PGM-Ni-Cu bearing intrusion measuring 2.9x 1.3km in area and measuring between 50-750m thick. The stratigraphy of the SLI based on the drilling to date can be broken down into 3 main units: Upper Gabbro Series, Lower Gabbroic Series and Ultramafic Series. Mineralization is observed to occur primarily in the Ultramafic Series which hosts the mineralized zone. The PGM-Cu-Ni mineralized zone now measures 700m long from depths of 370-800m. This zone remains open along and across strike and to date only ~ 10% of the intrusion has been tested with drilling. The morphology of the SLI is affected by the composition of the surrounding Archean country rocks which are metasediments and granodiorite. The contact between these two units is gradational, occurring over a width of up to 500m, where dykes or bands of granodiorite are observed to intrude the sediments. This transitional zone acts as a physical barrier to the SLI, changing its morphology to a structurally controlled dyke or chonolith as opposed to the lopolithic shape inferred for the main mass of the intrusion. In the MCR, massive sulfides are observed to occur within magma conduits at the Eagle Deposit in Michigan, the Tamarack Intrusion in Minnesota and isolated zones within the Thunder Bay North deposit. As such, the potential for the SLI to host base metal and PGM-rich massive sulfides should be considered during future exploration programs. Future work will require additional step-out diamond drill programs to define the extent of the PGM-Cu- Ni mineralized zone which remains open. Due to the conductive nature of magmatic sulfide assemblages borehole EM and/or borehole IP should be deployed to help guide drilling. This will be particularly important when expanding the zone into deeper ground.

Signatures

Appendix A: Diamond Drill Logs

Hole Number SL-14-006 Project Name: Project Code: Location: Start Date: Completed Date: Contractor: Core Storage: Units: Project SUNDAY LAKE 23 Nov 12, 2014 Nov 28, 2014 Orbit Garant TMC Core Shack METRIC Coordinates Primary Coordinates Grid: UTM83-16 North: 5,394,958.00 East: 334,842.00 Elev: 489.00 Destination Coordinates Grid: LL83 North: 48.69 East: -89.24 Elev: 489.00 Collar Collar Dip: -85.00 Collar Az: 270.00 Length: Hole Size: Hole Type: 863.00 NQ DD Casing: Left in Hole Collar Survey: N Plugged: N Multishot Survey: N Pulse EM Survey: N Detailed Lithology From To Lithology 0.00 1.80 CAS, CASING AND OVERBURDEN 1.80 90.30 MQZT, Mafic metasediment QUETICO METASEDIMENTARY ROCKS. WEAKLY BANDED QUETICO WITH PATCHY HEMATITE ALTERATION THROUGHOUT. ALTERATION OCCURS AS DEEP RED STAINING ALONG FRACTURES AND QUARTZ RICH BANDS OR AS A PERVASSIVE RED STAINING. WEAK FRACTURE FILLING EPIDOTE ALTERATION FOUND ALONG SOME BRITTLE FRACTURES. Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 1 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology 4.50-5.90: Hematite, Patchy, Moderate DISCREET ZONES OF RED QUETICO, ALTERATION ORIENTED ~85 DTCA 15.70-28.20: Hematite, Pervasive, Weak PREFERENTIALY ALTERS LEUCOSOME THROUGH THIS ZONE. ALTERATION FOLLOWS BANDING 28.20-35.40: Hematite, Pervasive, Moderate PERVASSIVE RED STAINING OF CORE THROUGH THIS INTERVAL, LOCALLY STRONG IN QUARTZ RICH SECTIONS. 35.40-38.20: Hematite, Pervasive, Weak 51.20-86.00: Hematite, Pervasive, Moderate PERVASSIVE RED STAINING OF CORE, LOCALLY STRONG IN QUARTZ RICH SECTIONS. 51.70-55.60: Epidote, Fracture Filling, Weak DOMINANTLY FOUND ALONG BRITTLE FRACTURE PLANES BUT ALSO WITHIN QUARTZ AND HEMATITE RICH ZONES 86.00-87.80: Hematite, Pervasive, Strong STRONG ALTERATION CONCENTRATED ALONG QUARTZ BAND AND FRACTURES 86.20-87.00: Epidote, Fracture Filling, Moderate 87.80-90.30: Hematite, Pervasive, Moderate Mineralization: 1.80-90.30: Pyrite, Fracture Filling, 1-2% Structure: 1.80-90.30: Banded 1.80-63.00: Banded WEAKLY BANDED TO BEDDED 1.80-63.00: Medium Grained 86.20-87.00: Broken Core STRONGLY HEMATIZED WITH MODERATE EPIDOTE ALTERATION Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 90.30 90.70 IMD, Mafic dykes DARK GREEN, ARCHEAN MAFIC DYKE. CHLORITE, BIOTITE WITH PORPHYROBLASTIC COARSE GRAINED GREEN FELDSPAR? MODERATELY HEMATIZED. 90.30-90.70: Chlorite, Pervasive, Strong 90.30-90.70: Hematite, Pervasive, Moderate Mineralization: 90.30-90.70: Pyrite, Fracture Filling, 1-2% Structure: 90.30-90.70: Contact Page 2 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology 90.30-90.70: Porphyroblastic 90.30-90.70: Schistose Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 90.70 92.20 MQZT, Mafic metasediment QUETICO METASEDIMENTARY ROCKS. MAROON COLOUR DUE TO PERVASSIVE MODERATE HEMATITE ALTERATION. SHARP CONTACTS WITH ADJACENT MAFIC DYKES ARE AT A LOW ANGLE TO BEDDING/BANDING. 90.70-92.20: Sericite, Fracture Filling, Weak BLEACHED HALOS AROUND FRACTURES 90.70-92.20: Hematite, Pervasive, Moderate Mineralization: 90.70-92.20: Pyrite, Fracture Filling, 1-2% Structure: 90.70-92.20: Banded 90.70-92.20: Banded 90.70-92.20: Medium Grained 92.20 92.60 IMD, Mafic dykes ARCHEAN MAFIC DYKE. SAME COMPOSITION AS DYKE INTERSECTED EARLIER. 92.20-92.60: Chlorite, Pervasive, Strong 92.20-92.60: Hematite, Pervasive, Moderate Structure: 92.20-92.20: Contact UPPER CONTACT 92.20-92.60: Foliation SHISTOSE FABRIC 92.60-92.60: Contact LOWER CONTACT 92.20-92.60: Schistose 92.20-92.60: Porphyroblastic 92.60 308.00 MQZT, Mafic metasediment Page 3 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology QUETICO METASEDIMENTARY ROCKS. WEAKLY BANDED QUETICO WITH PATCHY HEMATITE ALTERATION TO 197.4m. ALTERATION IS STRONGEST IN QUARTZ RICH ZONES, AND IN BROKEN/VUGGY SECTIONS OF CORE. CARBONATE AND CHLORITE ALTERATION OBSERVED ALONG SOME FRACTURES. VUGGY ZONES FROM 99.2-116.4m AND 126.5-127.3m HAVE PINK-RED SELF TERMINATING QUARTZ CRYSTALS IN OPEN SPACES. PORPHYROBLASTIC BLUE KYANITE? FOUND FROM 98-116m GIVING CORE A SPOTTED APPEARANCE. PORPHYROBLASTIC GARNET OBSERVED IN ISOLATED BEDS THROUGHOUT INTERVAL AND IS PINK-WHITE IN COLOUR, EUHEDRAL AND MEDIUM GRAINED. FROM 197.4m TO 298.1m CORE TAKES ON A GREY COLOUR WITH MINOR FRACTURE CONTROLLED SERICITE? ALTERATION (BLEACHED HALOS AROUND FRACTURES). FROM 275.2-277.6 A WHITE BED OF SILICOUS SEDIMENTS IS PRESENT. FROM 263.5-308m BANDING IS NEARLY ABSENT, GIVING THE CORE A MORE MASSIVE APPEARANCE. Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 4 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology 92.60-130.00: Hematite, Pervasive, Moderate VARIABLY HEMATIZED THROUGHOUT. ZONES OF STRONG ALTERATION INDICATED BELOW 92.60-308.00: Sericite, Fracture Filling, Weak BLEACHED HALOS SURROUNDING FINE FRACTURES 99.20-116.40: Chlorite, Fracture Filling, Moderate 99.20-116.40: Carbonate, Fracture Filling, Weak 112.50-113.50: Hematite, Pervasive, Strong 126.50-127.30: Carbonate, Fracture Filling, Moderate 126.50-127.30: Hematite, Pervasive, Strong 141.00-160.40: Hematite, Pervasive, Moderate ISOLATED ZONES OF STRONG ALTERATION WITHIN 154.90-155.80: Chlorite, Pervasive, Strong CHLORITE/QUARTZ RICH ZONE 160.40-169.50: Hematite, Pervasive, Weak 169.50-173.00: Hematite, Pervasive, Moderate 169.50-173.00: Epidote, Pervasive, Moderate 170.80-171.30: Epidote, Pervasive, Moderate 170.80-171.30: Chlorite, Pervasive, Strong 188.00-188.80: Hematite, Fracture Filling, Moderate 196.40-197.40: Hematite, Pervasive, Strong 197.40-199.60: Hematite, Pervasive, Moderate ALTERATION GRADUALLY FADES OUT 219.75-219.90: Chlorite, Fracture Filling, Weak BLEACHED FRACTURED ZONE 219.75-219.90: Hematite, Fracture Filling, Weak BLEACHED, FRACTURED ZONE 243.60-243.80: Hematite, Fracture Filling, Weak BLEACHED PINK COLOUR 249.30-249.40: Hematite, Fracture Filling, Weak BLEACHED PINK COLOUR 298.10-303.30: Hematite, Pervasive, Weak ALTERATION IS STRONGER WITHIN FRACTURES IN THIS INTERVAL 303.30-308.00: Hematite, Pervasive, Strong NARROW BRECCIA ZONE FOLLOWED BY DEEP RED STAINING OF CORE TO CONTACT WITH DYKE 303.40-303.60: Sericite, Fracture Filling, Strong SERICITIC ALTERATION WITHIN BRECCIA ZONE MATRIX 303.40-303.60: Chlorite, Fracture Filling, Strong CHLORITIC MATRIX TO BRECCIA ZONE 305.60-305.85: Chlorite, Fracture Filling, Strong Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 5 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology 307.40-308.00: Carbonate, Fracture Filling, Weak 307.40-308.00: Chlorite, Pervasive, Strong CHLORITIC ALTERATION WITHIN QUARTZ RICH ZONE Mineralization: 92.60-305.60: Pyrite, Fracture Filling, 1-2% 305.60-305.85: Pyrite, Disseminated, 4% Structure: 92.60-134.00: Banded 140.90-140.90: Banded 182.00-182.00: Banded 204.90-204.90: Banded 231.00-231.00: Banded 275.00-275.00: Bedded 92.60-263.50: Banded 98.00-116.00: Porphyroblastic COARSE GRAINED KYANITE 104.80-105.10: Broken Core 112.50-113.50: Fractured FRACTURED/VUGGY 126.50-127.30: Fractured FRACTURED WITH MINOR BROKEN CORE 142.40-143.10: Fractured FRACTURED/VUGGY 168.30-169.00: Porphyroblastic COARSE GRAINED KYANITE 196.40-197.40: Fractured FRACTURED/VUGGY 241.20-241.70: Pegmatitic QUARTZ RICH PEGMATITE VEIN 259.80-263.50: Pegmatitic QUARTZ RICH PEGMATITE VEIN 263.50-308.00: Bedded MORE BEDDED TEXTURE, BANDING NEARLY ABSENT AFTER PEGMATITE VEINS 303.40-303.60: Brecciated STRONGLY ALTERED BRECCIA ZONE Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 308.00 309.00 IMD, Mafic dykes ARCHEAN MAFIC DYKE. AMPHIBOLE + CHLORITE COMPOSITION. SHARP CONTACTS WITH STRONGLY HEMATIZED SEDIMENTS. DYKE IS ONLY WEAKLY ALTERED AT CONTACT. Page 6 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology 308.00-308.10: Hematite, Pervasive, Weak Structure: 308.00-308.00: Contact 309.00-309.00: Contact 308.00-309.00: Foliated 308.00-309.00: Fine Grained Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 309.00 414.05 MQZT, Mafic metasediment QUETICO METASEDIMENTARY ROCKS. MASSIVE TO BEDDED TO 321m THEN BACK TO A STRONGER GNEISSIC TEXTURE TO 340.9m. QUARTZ RICH BEDS FROM 315.5-318m AND 334.2-335.3m ARE WHITE IN COLOUR. STRONG HEMATITE ALTERATION AGAIN FROM 350.3-353.1m. RELATIVELY UNALTERED FROM 353.1-399.6m. FROM 399.6 TO LOWER CONTACT AT 414.05m HEMATITE ALTERATION RETURNS, STAINING CORE RED. LATE FRACTURES ARE MORE STRONGLY HEMATITE AND CHLORITE ALTERED AND TRUNCATE PERVASSIVE ALTERATION. PYRITE MINERALIZATION FROM 406.2m IS ASSOCIATED WITH THESE LATE FRACTURES AND CHLORITE RICH PODS. DIFFUSE CONTACT WITH UNDERLYING GABBRO BRECCIA, AS WIDENING FRACTURES BEGIN TO LOOK GABBROIC, ENCLOSING QUARTZ FRAGMENTS. QUARTZ FRAGMENTS APPEAR TO BE SOURCED FROM BANDS IN SEDIMENTS, WITH SURROUNDING SEDIMENT BEING DISSOLVED/ASSIMILATED INTO MAGMA. 309.00-310.00: Hematite, Pervasive, Strong DEEP RED STAINING TO CORE BUT ALSO CROSS CUTTING FRACTURES BLEACHING THIS COLOUR 310.00-311.00: Hematite, Fracture Filling, Moderate HEMATITE CONFINED TO FRACTURES WHILE REST OF CORE IS BLEACHED 320.00-321.60: Hematite, Pervasive, Moderate 321.20-321.60: Chlorite, Pervasive, Moderate 350.30-353.10: Hematite, Pervasive, Strong 365.40-365.50: Hematite, Fracture Filling, Strong 381.10-383.70: Hematite, Pervasive, Weak MAROON STAINING 399.60-414.05: Hematite, Pervasive, Strong DARK RED STAINING ON CORE, INTENSIFYING AS CONTACT IS APPROACHED 399.60-414.05: Chlorite, Fracture Filling, Moderate ASSOCIATED WITH HEMATITE FRACTURES. BECOMING STRONGER AS CONTACT IS APPROACHED 405.30-414.05: Hematite, Fracture Filling, Strong DEEP RED FRACTURES TRUNCATE BEDDING AND PERVASSIVE ALTERATION. ORIENTED ~85 DTCA AND ASSOCIATED WITH PYRITE IN SOME LOCATIONS N500599 407.00 408.00 1.00 91.000 57.000 29.000 0.005 0.003 0.001 0.500 N500600 408.00 409.00 1.00 95.000 62.000 26.000 0.005 0.003 0.001 0.500 N500601 409.00 410.00 1.00 85.000 185.000 23.000 0.005 0.003 0.001 0.500 N500602 410.00 411.00 1.00 84.000 81.000 26.000 0.005 0.003 0.001 0.500 N500603 411.00 412.00 1.00 93.000 60.000 24.000 0.005 0.002 0.001 0.500 N500604 412.00 413.00 1.00 86.000 13.000 25.000 0.005 0.002 0.001 0.500 N500605 413.00 414.05 1.05 78.000 24.000 23.000 0.005 0.002 0.001 0.500 Page 7 of 27 Feb 13, 2015

Hole Number: SL-14-006 From Mineralization: To Lithology 309.00-395.00: Pyrite, Fracture Filling, 1% FOUND ALONG BAND PARALLEL FRACTURE PLANES 395.00-406.20: Pyrite, Fracture Filling, 2% ASSOCIATED WITH LATE BRITTLE FRACTURES. SOMETIMES FOUND ALONG HEMATIZED FRACTURES. 406.20-407.40: Pyrite, Disseminated, 3% FINELY DISSEMINATED PYRITE WITHIN SEDIMENTS. RARE BLEBS OF PYRITE WITHIN CHLORITIC PATCHES Structure: 329.00-329.00: Banded 405.30-414.05: Fractured HEMATITE AND PYRITE FRACTURES 412.90-414.05: Brecciation QUARTZ BANDS BECOMING FRAGMENTED, DETACHED FROM EACH OTHER AS CONTACT IS APPROACHED 309.00-321.00: Bedded 321.00-340.90: Banded 340.90-359.00: Bedded 351.80-352.40: Brecciated HEMATITZED BRECCIA ZONE 359.00-414.05: Banded Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 414.05 416.00 IGBX, Gabbro Breccia DEEP RED GABBROIC BRECCIA. XENOLITHIC, TAXITIC TEXTURE WITH ANGULAR FRAGMENTS OF QUARTZ SURROUNDED BY A RED GABBRO MATRIX. QUARTZ FRAGMENTS COMPRISE 15% OF COMPOSITION, AND ARE SURROUNDED BY A CORONA OF CHLORITE. PYRITE FOUND WITHIN CHLORITIC HALOS. MINOR FRAGMENTS OF RELICT SEDIMENT ARE ALSO ANGULAR BUT NEARLY COMPLETELY DIGESTED. GROUNDMASS IS FINE GRAINED, MOTTLED, WITH MINOR AMPHIBOLE OBSERVED. SHARP CONTACT WITH UNDERLYING MONZOGABBRO. 414.05-416.00: Hematite, Pervasive, Strong Mineralization: 414.05-416.00: Pyrite, Disseminated, 2% 414.05-416.00: Xenolithic ANGULAR TO SUBANGULAR QUARTZ XENOLITHS THROUGHOUT 414.05-416.00: Varitextured N500606 414.05 415.00 0.95 66.000 29.000 22.000 0.005 0.003 0.001 0.500 N500607 415.00 416.00 1.00 47.000 50.000 22.000 0.005 0.005 0.001 0.500 416.00 692.80 IGUS, Upper Series Gabbro Page 8 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500608 416.00 417.00 1.00 1.000 12.000 15.000 0.005 0.001 0.001 0.500 N500608 416.00 417.00 1.00 1.000 12.000 15.000 0.005 0.001 0.001 0.500 N500609 417.00 418.00 1.00 1.000 5.000 17.000 0.005 0.001 0.001 0.500 N500609 417.00 418.00 1.00 1.000 5.000 17.000 0.005 0.001 0.001 0.500 N500611 418.00 419.00 1.00 2.000 8.000 19.000 0.005 0.001 0.001 0.500 N500611 418.00 419.00 1.00 2.000 8.000 19.000 0.005 0.001 0.001 0.500 N500612 419.00 420.00 1.00 1.000 4.000 17.000 0.005 0.001 0.001 0.500 N500612 419.00 420.00 1.00 1.000 4.000 17.000 0.005 0.001 0.001 0.500 N500613 420.00 421.00 1.00 1.000 7.000 23.000 0.005 0.001 0.001 0.500 N500613 420.00 421.00 1.00 1.000 7.000 23.000 0.005 0.001 0.001 0.500 N500614 421.00 422.00 1.00 1.000 2.000 20.000 0.005 0.001 0.001 0.500 N500614 421.00 422.00 1.00 1.000 2.000 20.000 0.005 0.001 0.001 0.500 N500615 422.00 423.50 1.50 1.000 73.000 29.000 0.005 0.001 0.001 0.500 N500615 422.00 423.50 1.50 1.000 73.000 29.000 0.005 0.001 0.001 0.500 N500616 423.50 425.00 1.50 1.000 47.000 38.000 0.005 0.001 0.001 0.500 N500616 423.50 425.00 1.50 1.000 47.000 38.000 0.005 0.001 0.001 0.500 N500617 425.00 426.50 1.50 1.000 2.000 35.000 0.005 0.001 0.001 0.500 N500617 425.00 426.50 1.50 1.000 2.000 35.000 0.005 0.001 0.001 0.500 N500618 426.50 428.00 1.50 1.000 48.000 34.000 0.005 0.001 0.001 0.500 N500618 426.50 428.00 1.50 1.000 48.000 34.000 0.005 0.001 0.001 0.500 N500619 438.00 439.50 1.50 19.000 192.000 41.000 0.005 0.001 0.001 0.500 N500619 438.00 439.50 1.50 19.000 192.000 41.000 0.005 0.001 0.001 0.500 N500621 448.00 449.50 1.50 2.000 69.000 32.000 0.005 0.001 0.001 0.500 N500621 448.00 449.50 1.50 2.000 69.000 32.000 0.005 0.001 0.001 0.500 N500622 458.00 459.50 1.50 1.000 20.000 28.000 0.005 0.001 0.001 0.500 N500622 458.00 459.50 1.50 1.000 20.000 28.000 0.005 0.001 0.001 0.500 N500623 468.00 469.50 1.50 1.000 19.000 22.000 0.005 0.001 0.001 0.500 N500623 468.00 469.50 1.50 1.000 19.000 22.000 0.005 0.001 0.001 0.500 N500624 478.00 479.50 1.50 1.000 15.000 15.000 0.005 0.001 0.001 0.500 N500624 478.00 479.50 1.50 1.000 15.000 15.000 0.005 0.001 0.001 0.500 N500625 488.00 489.50 1.50 1.000 14.000 14.000 0.005 0.001 0.001 0.500 N500625 488.00 489.50 1.50 1.000 14.000 14.000 0.005 0.001 0.001 0.500 N500626 498.00 498.50 0.50 1.000 25.000 12.000 0.005 0.001 0.001 0.500 N500626 498.00 498.50 0.50 1.000 25.000 12.000 0.005 0.001 0.001 0.500 N500627 508.00 509.50 1.50 1.000 14.000 13.000 0.005 0.001 0.001 0.500 N500627 508.00 509.50 1.50 1.000 14.000 13.000 0.005 0.001 0.001 0.500 N500628 518.00 519.50 1.50 1.000 10.000 10.000 0.005 0.001 0.001 0.500 N500628 518.00 519.50 1.50 1.000 10.000 10.000 0.005 0.001 0.001 0.500 N500629 528.00 529.50 1.50 1.000 9.000 10.000 0.005 0.001 0.001 0.500 N500629 528.00 529.50 1.50 1.000 9.000 10.000 0.005 0.001 0.001 0.500 N500631 538.00 539.50 1.50 3.000 8.000 12.000 0.005 0.001 0.001 0.500 N500631 538.00 539.50 1.50 3.000 8.000 12.000 0.005 0.001 0.001 0.500 N500632 548.00 549.50 1.50 1.000 1.000 26.000 0.005 0.001 0.001 0.500 N500632 548.00 549.50 1.50 1.000 1.000 26.000 0.005 0.001 0.001 0.500 N500633 558.00 559.50 1.50 1.000 9.000 21.000 0.005 0.001 0.001 0.500 N500634 568.00 569.50 1.50 1.000 14.000 32.000 0.005 0.001 0.001 0.500 Page 9 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500635 569.50 571.00 1.50 1.000 18.000 38.000 0.005 0.001 0.001 0.500 N500636 571.00 572.00 1.00 1.000 24.000 51.000 0.005 0.001 0.001 0.500 N500637 572.00 573.00 1.00 3.000 16.000 27.000 0.005 0.001 0.001 0.500 N500638 573.00 574.00 1.00 5.000 21.000 36.000 0.005 0.001 0.001 0.500 N500639 574.00 575.00 1.00 1.000 32.000 48.000 0.005 0.001 0.001 0.500 N500640 574.00 575.00 1.00 3.000 30.000 51.000 0.005 0.001 0.001 0.500 N500641 575.00 576.00 1.00 3.000 16.000 46.000 0.005 0.001 0.001 0.500 N500642 576.00 577.00 1.00 3.000 25.000 41.000 0.005 0.001 0.001 0.500 N500643 577.00 578.00 1.00 1.000 23.000 45.000 0.005 0.001 0.001 0.500 N500644 578.00 579.00 1.00 1.000 27.000 49.000 0.005 0.001 0.001 0.500 N500645 579.00 580.00 1.00 1.000 23.000 37.000 0.005 0.001 0.001 0.500 N500646 580.00 581.00 1.00 2.000 21.000 38.000 0.005 0.001 0.001 0.500 N500647 581.00 582.00 1.00 1.000 19.000 37.000 0.005 0.001 0.001 0.500 N500648 582.00 583.00 1.00 1.000 22.000 49.000 0.005 0.001 0.001 0.500 N500649 588.00 589.50 1.50 1.000 32.000 40.000 0.005 0.001 0.001 0.500 N500651 598.00 599.50 1.50 5.000 53.000 51.000 0.005 0.001 0.001 0.500 N500652 608.00 609.50 1.50 9.000 68.000 54.000 0.005 0.001 0.001 0.500 N500653 618.00 619.50 1.50 15.000 238.000 59.000 0.005 0.001 0.001 0.500 N500654 628.00 629.50 1.50 37.000 423.000 63.000 0.005 0.001 0.001 0.500 N500655 638.00 639.50 1.50 65.000 524.000 67.000 0.005 0.001 0.001 0.500 N500656 648.00 649.50 1.50 122.000 698.000 82.000 0.005 0.001 0.001 0.500 N500657 658.00 659.50 1.50 145.000 770.000 67.000 0.005 0.001 0.003 0.500 N500658 668.00 669.50 1.50 89.000 263.000 41.000 0.005 0.001 0.004 0.500 N500659 678.00 679.50 1.50 116.000 308.000 47.000 0.005 0.001 0.016 0.500 N500661 688.00 689.00 1.00 124.000 287.000 43.000 0.145 0.012 0.025 0.500 N500662 689.00 690.00 1.00 124.000 300.000 42.000 0.168 0.017 0.038 0.500 N500663 690.00 691.00 1.00 118.000 351.000 41.000 0.320 0.045 0.046 0.500 N500664 691.00 692.00 1.00 128.000 307.000 42.000 0.191 0.024 0.032 0.500 N500665 692.00 692.80 0.80 144.000 283.000 46.000 0.200 0.032 0.019 0.500 N500634 568.00 569.50 1.50 1.000 14.000 32.000 0.005 0.001 0.001 0.500 N500635 569.50 571.00 1.50 1.000 18.000 38.000 0.005 0.001 0.001 0.500 N500636 571.00 572.00 1.00 1.000 24.000 51.000 0.005 0.001 0.001 0.500 N500637 572.00 573.00 1.00 3.000 16.000 27.000 0.005 0.001 0.001 0.500 N500638 573.00 574.00 1.00 5.000 21.000 36.000 0.005 0.001 0.001 0.500 N500639 574.00 575.00 1.00 1.000 32.000 48.000 0.005 0.001 0.001 0.500 N500640 574.00 575.00 1.00 3.000 30.000 51.000 0.005 0.001 0.001 0.500 N500641 575.00 576.00 1.00 3.000 16.000 46.000 0.005 0.001 0.001 0.500 N500642 576.00 577.00 1.00 3.000 25.000 41.000 0.005 0.001 0.001 0.500 N500643 577.00 578.00 1.00 1.000 23.000 45.000 0.005 0.001 0.001 0.500 N500644 578.00 579.00 1.00 1.000 27.000 49.000 0.005 0.001 0.001 0.500 N500645 579.00 580.00 1.00 1.000 23.000 37.000 0.005 0.001 0.001 0.500 N500646 580.00 581.00 1.00 2.000 21.000 38.000 0.005 0.001 0.001 0.500 N500647 581.00 582.00 1.00 1.000 19.000 37.000 0.005 0.001 0.001 0.500 N500648 582.00 583.00 1.00 1.000 22.000 49.000 0.005 0.001 0.001 0.500 N500649 588.00 589.50 1.50 1.000 32.000 40.000 0.005 0.001 0.001 0.500 N500651 598.00 599.50 1.50 5.000 53.000 51.000 0.005 0.001 0.001 0.500 Page 10 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500652 608.00 609.50 1.50 9.000 68.000 54.000 0.005 0.001 0.001 0.500 N500653 618.00 619.50 1.50 15.000 238.000 59.000 0.005 0.001 0.001 0.500 N500654 628.00 629.50 1.50 37.000 423.000 63.000 0.005 0.001 0.001 0.500 N500655 638.00 639.50 1.50 65.000 524.000 67.000 0.005 0.001 0.001 0.500 N500656 648.00 649.50 1.50 122.000 698.000 82.000 0.005 0.001 0.001 0.500 N500657 658.00 659.50 1.50 145.000 770.000 67.000 0.005 0.001 0.003 0.500 N500658 668.00 669.50 1.50 89.000 263.000 41.000 0.005 0.001 0.004 0.500 N500659 678.00 679.50 1.50 116.000 308.000 47.000 0.005 0.001 0.016 0.500 N500661 688.00 689.00 1.00 124.000 287.000 43.000 0.145 0.012 0.025 0.500 N500662 689.00 690.00 1.00 124.000 300.000 42.000 0.168 0.017 0.038 0.500 N500663 690.00 691.00 1.00 118.000 351.000 41.000 0.320 0.045 0.046 0.500 N500664 691.00 692.00 1.00 128.000 307.000 42.000 0.191 0.024 0.032 0.500 N500665 692.00 692.80 0.80 144.000 283.000 46.000 0.200 0.032 0.019 0.500 MINOR INTERVALS: 416.00-558.50 : ILGB Leucogabbro MONZOGABBRO TO LEUCOGABBRO. COARSE GRAINED ACICULAR AMPHIBOLE FROM 416-420.1m AND AGAIN AT 429.8-449m. STRONG PERVASSIVE HEMATITE ALTERATION FROM 416-558.5m. STRONGEST FROM 416-421.6m AND FROM 525.2-558.5m WHERE THE GROUNDMASS IS VERY FINE GRAINED, RED AND ANHEDRAL, SURROUNDING MEDIUM TO COARSE GRAINED AMPHIBOLE AND MINOR FELDSPAR. SHARP INTERNAL CONTACT AT 412.6m WHERE HEMATITE ALTERATION DECREASES SLIGHTLY AND COARSE GRAINED LATHS OF PLAGIOCLASE APPEAR. PLAGIOCLASE ARE MODERATELY SERICITIZED GIVING THEM A GREEN COLOUR. FROM 421.6-435.5m CORE TAKES A SPOTTED TEXTURE WITH GREEN AND RED SPOTS DUE TO HEMATITE-EPIDOTE-SERICITE ALTERATION. CHLORITE ALTERATION FOUND ALONG MOST FRACTURES. MINOR, THIN VEINS OF CARBONATE CROSS CUT THE GABBRO. SUBANGULAR, FINE TO MEDIUM GRAINED CARBONATE OCELLI ARE FOUND FROM 441.2-557m. 2-3% DISSEMINATED PYRITE FROM 416-424.3m, THEN 1% DISSEMINATED PYRITE THROUGH REST OF INTERVAL. CORE BECOMES PITTED FROM 518-558.5m. EXTREMELY PITTED AND CRUMBLY FROM 548-549.3m. LOWER CONTACT MARKED WHERE HEMATITE ALTERATION WEAKENS AND AND EUHEDRAL PLAGIOCLASE AND PYROXENE ARE CUMULATE PHASES. 558.50-692.80 : IGB Gabbro COARSE GRAINED GABBRO/OXIDE GABBRO. ADCUMULATE PLAGIOCLASE AND PYROXENE ARE DOMINANT MINERALS (50-65% PLAGIOCLASE-35-50% PYROXENE). HEMATITE ALTERATION PERSISTS AS A LIGHT RED CORONA SURROUNDING EUHEDRAL PLAGIOCLASE. EPIDOTE ALTERATION IS VARIABLE THROUGHOUT, OCCURING AS WEAK SPOTS OR WITHIN VEINS. 1-2% DISSEMINATED PYRITE FOUND THROUGHOUT, OFTEN ASSOCIATED WITH CHLORITIC PATCHES. IGNEOUS LAYERING PRESENT FROM 558.5-582.6m. FROM 579.5-580.3m, 1-2cm THICK OXIDE RICH HORIZONS ARE FOUND AT THE BOTTOM OF LAYERS. FROM 602m-692.5m PROMINENT DULL WHITE COLOURED SPOTS ARE OBSERVED. THESE SPOTS APPEAR TO BE ALTERED FROM SERICITIZED PLAGIOCLASE.. POSSIBLY A SODIC RICH PHASE? Page 11 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Minor Lithology 416.00-539.00: Chlorite, Fracture Filling, Moderate 416.00-558.50: Hematite, Pervasive, Strong 421.60-511.50: Sericite, Pervasive, Moderate GREEN STAINING OF FELDSPAR. GRADUALLY WEAKENS UNTIL FELDSPAR APPEAR WHITE 441.20-557.00: Carbonate, Spots, Weak ROUNDED TO ANGULAR CARBONATE SPOTS CAN SHOW NARROW HALOS OF HEMATITE OR CHLORITE. MINOR FRACTURE FILLING CARBONATE AS WELL 441.20-558.50: Epidote, Fracture Filling, Weak OCCAISONAL EPIDOTE AND CHLORITE PATCHES 554.10-558.50: Sericite, Pervasive, Moderate SERICITIZED PLAGIOCLASE 558.50-558.50: Hematite, Pervasive, Moderate HEMATITE CONFINED TO HALOS AROUND EUHEDRAL PLAGIOCLASE AND MINOR INTERCUMULUS GROUNDMASS 558.50-582.50: Hematite, Pervasive, Moderate 558.50-600.30: Epidote, Pervasive, Weak 558.50-644.00: Hornblende, Pervasive, Strong ALL PYROXENE ARE ALTERED TO AMPHIBOLE/CHLORITE 582.50-644.00: Hematite, Pervasive, Weak RED HALOS SURROUNDING PLAGIOCLASE CRYSTALS 584.00-590.00: Chlorite, Spots, Moderate CHLORITIC PHENOCRYSTS APPEAR TO BE RELICT PYROXENE. ASSOCIATED WITH PYRITE MINERALIZATION Minor Mineralization: 416.00-424.30: Pyrite, Disseminated, 2-3% ALSO FOUND IN NARROW FRACTURES NEAR UPPER CONTACT 419.00-558.50: Magnetite, Disseminated, 2-5% 424.30-558.50: Pyrite, Disseminated, 1% 558.50-644.00: Magnetite, Disseminated, 5% 558.50-644.00: Pyrite, Disseminated, 1-2% 579.50-580.30: Magnetite, Cumulus, 10% 1-2cm THICK OXIDE RICH HORIZONS AT BASE OF LAYERS Minor Structure: 558.50-582.60: Igneous Layering LAYERS ARE 5-50cm WIDE. Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 12 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Minor Lithology 416.00-509.80: Medium Grained - Coarse Grained GRAINSIZE IS SLIGHTLY VARIABLE 416.00-558.50: Massive ISOLOATED ZONES OF CUMULATE PLAGIOCLASE BUT LARGELY MASSIVE TEXTURE WITH COARSE GRAINED AMPHIBOLE SURROUNDED BY ANHEDRAL RED GROUNDMASS 509.80-526.00: Coarse Grained COARSE GRAINED CUMULATE PLAGIOCLASE AND AMPHIBOLE 518.00-539.00: Glomerophyric RADIAL AMPHIBOLE 526.00-530.90: Medium Grained - Coarse Grained 530.90-558.50: Coarse Grained 558.50-582.60: Foliated IGNEOUS FOLIATION DUE TO LAYERING. OBSERVED AS PLAGIOCLASE ORIENTATION 558.50-635.00: Mesocumulate CUMULATE PHASES ARE PLAGIOCLASE AND CLINOPYROXENE 558.50-644.00: Coarse Grained MINOR GRAINSIZE VARIATIONS BUT OVERALL COARSE GRAINED 635.00-644.00: Subophitic TEXTURE SLOWLY CHANGES FROM CUMULATE/INTERGRANULAR TO SUBOPHITIC 638.00-644.00: Foliated IGNEOUS FOLIATION Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 692.80 806.40 IGLS, Lower Series Gabbro Page 13 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology FRACTIONATED SEQUENCE OF INTRUSIVES WITH A CORE OF PERIDOTITE SURROUNDED BY MORE EVOLVED GABBROIC ROCKS. DIFFUSE CONTACTS BETWEEN UNITS GRADUALLY CHANGE IN COMPOSITION. MAGMATIC SULFIDE MINERALIZATION OBSERVED NEAR THE UPPER CONTACT OF THE UNIT AND WITHIN THE LOWER OLIVINE MELAGABBRO UNITS. GENERALLY MASSIVE AND HOMOGENOUS IN APPEARANCE. MINOR CHLORITIC FRACTURES RARELY SHOWING SLICKENLINES. FAULTED LOWER CONTACT WITH ULTRAMAFIC SERIES. Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500666 692.80 694.00 1.20 190.000 202.000 57.000 0.337 0.140 0.029 0.500 N500666 692.80 694.00 1.20 190.000 202.000 57.000 0.337 0.140 0.029 0.500 N500667 694.00 695.00 1.00 213.000 191.000 67.000 0.387 0.272 0.034 0.500 N500667 694.00 695.00 1.00 213.000 191.000 67.000 0.387 0.272 0.034 0.500 N500668 695.00 696.00 1.00 256.000 141.000 71.000 0.338 0.246 0.004 0.500 N500668 695.00 696.00 1.00 256.000 141.000 71.000 0.338 0.246 0.004 0.500 N500669 696.00 697.00 1.00 235.000 122.000 67.000 0.288 0.168 0.001 0.500 N500669 696.00 697.00 1.00 235.000 122.000 67.000 0.288 0.168 0.001 0.500 N500671 697.00 698.00 1.00 208.000 82.000 60.000 0.256 0.144 0.002 0.500 N500671 697.00 698.00 1.00 208.000 82.000 60.000 0.256 0.144 0.002 0.500 N500672 698.00 699.00 1.00 169.000 70.000 54.000 0.157 0.122 0.001 0.500 N500672 698.00 699.00 1.00 169.000 70.000 54.000 0.157 0.122 0.001 0.500 N500673 699.00 700.00 1.00 167.000 54.000 56.000 0.089 0.095 0.002 0.500 N500673 699.00 700.00 1.00 167.000 54.000 56.000 0.089 0.095 0.002 0.500 N500674 700.00 701.00 1.00 181.000 76.000 58.000 0.096 0.099 0.001 0.500 N500674 700.00 701.00 1.00 181.000 76.000 58.000 0.096 0.099 0.001 0.500 N500675 701.00 702.00 1.00 194.000 80.000 62.000 0.144 0.100 0.001 0.500 N500675 701.00 702.00 1.00 194.000 80.000 62.000 0.144 0.100 0.001 0.500 N500676 702.00 703.00 1.00 195.000 79.000 59.000 0.053 0.069 0.001 0.500 N500676 702.00 703.00 1.00 195.000 79.000 59.000 0.053 0.069 0.001 0.500 N500677 703.00 704.00 1.00 198.000 86.000 60.000 0.032 0.021 0.001 0.500 N500677 703.00 704.00 1.00 198.000 86.000 60.000 0.032 0.021 0.001 0.500 N500678 704.00 705.00 1.00 225.000 83.000 65.000 0.021 0.015 0.001 0.500 N500678 704.00 705.00 1.00 225.000 83.000 65.000 0.021 0.015 0.001 0.500 N500679 705.00 706.00 1.00 195.000 56.000 61.000 0.013 0.011 0.001 0.500 N500680 705.00 706.00 1.00 194.000 57.000 61.000 0.014 0.012 0.001 0.500 N500679 705.00 706.00 1.00 195.000 56.000 61.000 0.013 0.011 0.001 0.500 N500680 705.00 706.00 1.00 194.000 57.000 61.000 0.014 0.012 0.001 0.500 N500681 706.00 707.00 1.00 182.000 83.000 59.000 0.028 0.028 0.002 0.500 N500681 706.00 707.00 1.00 182.000 83.000 59.000 0.028 0.028 0.002 0.500 N500682 707.00 708.00 1.00 216.000 90.000 64.000 0.015 0.015 0.001 0.500 N500683 708.00 709.00 1.00 233.000 86.000 67.000 0.013 0.011 0.001 0.500 N500684 709.00 710.00 1.00 246.000 92.000 68.000 0.013 0.009 0.001 0.500 N500685 710.00 711.50 1.50 271.000 104.000 73.000 0.009 0.004 0.001 0.500 N500686 711.50 713.00 1.50 259.000 103.000 71.000 0.029 0.012 0.001 0.500 N500687 713.00 714.50 1.50 309.000 112.000 77.000 0.015 0.008 0.002 0.500 N500688 714.50 716.00 1.50 341.000 89.000 82.000 0.012 0.005 0.001 0.500 N500689 716.00 717.50 1.50 348.000 72.000 82.000 0.019 0.008 0.002 0.500 N500691 717.50 719.00 1.50 346.000 82.000 84.000 0.011 0.004 0.001 0.500 N500692 719.00 720.50 1.50 364.000 72.000 86.000 0.008 0.003 0.001 0.500 N500693 720.50 722.00 1.50 396.000 71.000 91.000 0.012 0.004 0.001 0.500 N500694 722.00 723.50 1.50 401.000 62.000 89.000 0.008 0.004 0.001 0.500 N500695 723.50 725.00 1.50 409.000 52.000 91.000 0.016 0.004 0.001 0.500 N500696 725.00 726.50 1.50 422.000 64.000 92.000 0.020 0.008 0.001 0.500 N500697 726.50 728.00 1.50 414.000 60.000 92.000 0.006 0.005 0.001 0.500 N500698 728.00 729.50 1.50 401.000 53.000 90.000 0.008 0.002 0.001 0.500 Page 14 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500699 729.50 731.00 1.50 383.000 52.000 86.000 0.017 0.007 0.001 0.500 N500701 731.00 732.50 1.50 382.000 58.000 88.000 0.013 0.004 0.001 0.500 N500702 732.50 734.00 1.50 393.000 51.000 86.000 0.012 0.003 0.001 0.500 N500703 734.00 735.50 1.50 355.000 69.000 78.000 0.012 0.003 0.001 0.500 N500704 735.50 737.00 1.50 397.000 64.000 84.000 0.016 0.005 0.001 0.500 N500705 737.00 738.50 1.50 401.000 65.000 83.000 0.015 0.011 0.001 0.500 N500706 738.50 740.00 1.50 455.000 69.000 89.000 0.011 0.005 0.001 0.500 N500707 740.00 741.50 1.50 625.000 94.000 115.000 0.022 0.010 0.002 0.500 N500708 741.50 743.00 1.50 604.000 83.000 107.000 0.017 0.008 0.001 0.500 N500709 743.00 744.50 1.50 736.000 88.000 124.000 0.025 0.011 0.001 0.500 N500711 744.50 746.00 1.50 783.000 87.000 132.000 0.030 0.010 0.001 0.500 N500712 746.00 747.50 1.50 758.000 82.000 129.000 0.030 0.016 0.001 0.500 N500713 747.50 749.00 1.50 680.000 82.000 114.000 0.018 0.010 0.002 0.500 N500714 749.00 750.50 1.50 757.000 96.000 128.000 0.038 0.028 0.003 0.500 N500715 750.50 752.00 1.50 756.000 81.000 125.000 0.028 0.010 0.001 0.500 N500716 752.00 753.50 1.50 738.000 90.000 123.000 0.027 0.018 0.001 0.500 N500717 753.50 755.00 1.50 813.000 86.000 136.000 0.023 0.007 0.001 0.500 N500718 755.00 756.50 1.50 835.000 91.000 137.000 0.042 0.044 0.002 0.500 N500719 756.50 758.00 1.50 785.000 87.000 130.000 0.023 0.010 0.001 0.500 N500721 758.00 759.50 1.50 796.000 92.000 131.000 0.037 0.022 0.001 0.500 N500722 759.50 761.00 1.50 809.000 90.000 132.000 0.032 0.018 0.001 0.500 N500723 761.00 762.50 1.50 794.000 100.000 131.000 0.039 0.026 0.001 0.500 N500724 762.50 764.00 1.50 744.000 97.000 123.000 0.030 0.012 0.001 0.500 N500725 764.00 765.50 1.50 766.000 113.000 130.000 0.038 0.031 0.001 0.500 N500726 765.50 767.00 1.50 710.000 99.000 122.000 0.028 0.016 0.001 0.500 N500727 767.00 768.50 1.50 614.000 96.000 109.000 0.033 0.016 0.001 0.500 N500728 768.50 770.00 1.50 594.000 126.000 104.000 0.031 0.017 0.001 0.500 N500729 770.00 771.50 1.50 602.000 251.000 101.000 0.058 0.042 0.005 0.500 N500731 771.50 773.00 1.50 550.000 174.000 103.000 0.042 0.036 0.003 0.500 N500732 773.00 774.50 1.50 497.000 123.000 96.000 0.033 0.019 0.003 0.500 N500733 774.50 776.00 1.50 427.000 89.000 88.000 0.018 0.008 0.001 0.500 N500734 776.00 777.00 1.00 449.000 110.000 91.000 0.022 0.012 0.001 0.500 N500735 777.00 778.00 1.00 449.000 104.000 92.000 0.019 0.013 0.001 0.500 N500736 778.00 779.00 1.00 434.000 137.000 91.000 0.021 0.013 0.002 0.500 N500737 779.00 780.00 1.00 393.000 312.000 80.000 0.058 0.058 0.007 0.500 N500501 780.00 781.00 1.00 0.034 0.032 0.005 0.080 N500502 781.00 782.00 1.00 0.031 0.030 0.002 0.060 N500503 782.00 783.00 1.00 0.022 0.012 0.002 0.510 N500504 783.00 784.00 1.00 0.023 0.017 0.001 0.350 N500505 784.00 785.00 1.00 0.022 0.016 0.007 0.060 N500506 785.00 786.00 1.00 0.028 0.006 0.001 0.240 N500507 786.00 787.00 1.00 0.032 0.017 0.003 0.300 N500508 787.00 788.00 1.00 0.032 0.012 0.004 0.140 N500509 788.00 789.00 1.00 0.039 0.015 0.004 0.090 N500511 789.00 789.50 0.50 0.116 0.085 0.014 0.430 N500512 789.50 790.00 0.50 0.024 0.006 0.002 0.230 Page 15 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500513 790.00 791.00 1.00 0.022 0.016 0.002 0.130 N500514 791.00 791.50 0.50 0.092 0.065 0.008 0.520 N500515 791.50 792.00 0.50 0.017 0.004 0.001 0.070 N500516 792.00 793.00 1.00 0.022 0.011 0.002 0.120 N500517 793.00 794.00 1.00 0.028 0.021 0.002 0.230 N500519 794.00 795.00 1.00 0.014 0.006 0.001 0.110 N500520 795.00 796.00 1.00 0.036 0.005 0.001 0.160 N500521 796.00 797.00 1.00 0.029 0.005 0.001 0.100 N500522 797.00 798.00 1.00 0.028 0.007 0.001 0.040 N500523 798.00 799.00 1.00 0.018 0.007 0.001 0.070 N500524 799.00 800.00 1.00 0.013 0.006 0.002 0.040 N500525 800.00 801.00 1.00 0.011 0.009 0.001 0.060 N500526 801.00 802.00 1.00 0.011 0.007 0.001 0.020 N500527 802.00 803.00 1.00 0.018 0.012 0.001 0.020 N500528 803.00 804.00 1.00 0.022 0.022 0.003 0.020 N500529 804.00 805.00 1.00 0.046 0.067 0.016 0.020 N500531 805.00 806.00 1.00 0.045 0.027 0.003 0.030 N500532 806.00 806.40 0.40 0.116 0.097 0.012 0.040 N500682 707.00 708.00 1.00 216.000 90.000 64.000 0.015 0.015 0.001 0.500 N500683 708.00 709.00 1.00 233.000 86.000 67.000 0.013 0.011 0.001 0.500 N500684 709.00 710.00 1.00 246.000 92.000 68.000 0.013 0.009 0.001 0.500 N500685 710.00 711.50 1.50 271.000 104.000 73.000 0.009 0.004 0.001 0.500 N500686 711.50 713.00 1.50 259.000 103.000 71.000 0.029 0.012 0.001 0.500 N500687 713.00 714.50 1.50 309.000 112.000 77.000 0.015 0.008 0.002 0.500 N500688 714.50 716.00 1.50 341.000 89.000 82.000 0.012 0.005 0.001 0.500 N500689 716.00 717.50 1.50 348.000 72.000 82.000 0.019 0.008 0.002 0.500 N500691 717.50 719.00 1.50 346.000 82.000 84.000 0.011 0.004 0.001 0.500 N500693 720.50 722.00 1.50 396.000 71.000 91.000 0.012 0.004 0.001 0.500 N500694 722.00 723.50 1.50 401.000 62.000 89.000 0.008 0.004 0.001 0.500 N500695 723.50 725.00 1.50 409.000 52.000 91.000 0.016 0.004 0.001 0.500 N500696 725.00 726.50 1.50 422.000 64.000 92.000 0.020 0.008 0.001 0.500 N500697 726.50 728.00 1.50 414.000 60.000 92.000 0.006 0.005 0.001 0.500 N500698 728.00 729.50 1.50 401.000 53.000 90.000 0.008 0.002 0.001 0.500 N500699 729.50 731.00 1.50 383.000 52.000 86.000 0.017 0.007 0.001 0.500 N500701 731.00 732.50 1.50 382.000 58.000 88.000 0.013 0.004 0.001 0.500 N500702 732.50 734.00 1.50 393.000 51.000 86.000 0.012 0.003 0.001 0.500 N500703 734.00 735.50 1.50 355.000 69.000 78.000 0.012 0.003 0.001 0.500 N500704 735.50 737.00 1.50 397.000 64.000 84.000 0.016 0.005 0.001 0.500 N500705 737.00 738.50 1.50 401.000 65.000 83.000 0.015 0.011 0.001 0.500 N500706 738.50 740.00 1.50 455.000 69.000 89.000 0.011 0.005 0.001 0.500 N500707 740.00 741.50 1.50 625.000 94.000 115.000 0.022 0.010 0.002 0.500 N500708 741.50 743.00 1.50 604.000 83.000 107.000 0.017 0.008 0.001 0.500 N500709 743.00 744.50 1.50 736.000 88.000 124.000 0.025 0.011 0.001 0.500 N500712 746.00 747.50 1.50 758.000 82.000 129.000 0.030 0.016 0.001 0.500 N500713 747.50 749.00 1.50 680.000 82.000 114.000 0.018 0.010 0.002 0.500 N500714 749.00 750.50 1.50 757.000 96.000 128.000 0.038 0.028 0.003 0.500 Page 16 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500715 750.50 752.00 1.50 756.000 81.000 125.000 0.028 0.010 0.001 0.500 N500716 752.00 753.50 1.50 738.000 90.000 123.000 0.027 0.018 0.001 0.500 N500717 753.50 755.00 1.50 813.000 86.000 136.000 0.023 0.007 0.001 0.500 N500718 755.00 756.50 1.50 835.000 91.000 137.000 0.042 0.044 0.002 0.500 N500719 756.50 758.00 1.50 785.000 87.000 130.000 0.023 0.010 0.001 0.500 N500721 758.00 759.50 1.50 796.000 92.000 131.000 0.037 0.022 0.001 0.500 N500722 759.50 761.00 1.50 809.000 90.000 132.000 0.032 0.018 0.001 0.500 N500723 761.00 762.50 1.50 794.000 100.000 131.000 0.039 0.026 0.001 0.500 N500725 764.00 765.50 1.50 766.000 113.000 130.000 0.038 0.031 0.001 0.500 N500726 765.50 767.00 1.50 710.000 99.000 122.000 0.028 0.016 0.001 0.500 N500727 767.00 768.50 1.50 614.000 96.000 109.000 0.033 0.016 0.001 0.500 N500728 768.50 770.00 1.50 594.000 126.000 104.000 0.031 0.017 0.001 0.500 N500729 770.00 771.50 1.50 602.000 251.000 101.000 0.058 0.042 0.005 0.500 N500731 771.50 773.00 1.50 550.000 174.000 103.000 0.042 0.036 0.003 0.500 N500732 773.00 774.50 1.50 497.000 123.000 96.000 0.033 0.019 0.003 0.500 N500733 774.50 776.00 1.50 427.000 89.000 88.000 0.018 0.008 0.001 0.500 N500734 776.00 777.00 1.00 449.000 110.000 91.000 0.022 0.012 0.001 0.500 N500735 777.00 778.00 1.00 449.000 104.000 92.000 0.019 0.013 0.001 0.500 N500736 778.00 779.00 1.00 434.000 137.000 91.000 0.021 0.013 0.002 0.500 N500737 779.00 780.00 1.00 393.000 312.000 80.000 0.058 0.058 0.007 0.500 N500501 780.00 781.00 1.00 0.034 0.032 0.005 0.080 N500502 781.00 782.00 1.00 0.031 0.030 0.002 0.060 N500503 782.00 783.00 1.00 0.022 0.012 0.002 0.510 N500504 783.00 784.00 1.00 0.023 0.017 0.001 0.350 N500505 784.00 785.00 1.00 0.022 0.016 0.007 0.060 N500506 785.00 786.00 1.00 0.028 0.006 0.001 0.240 N500507 786.00 787.00 1.00 0.032 0.017 0.003 0.300 N500508 787.00 788.00 1.00 0.032 0.012 0.004 0.140 N500509 788.00 789.00 1.00 0.039 0.015 0.004 0.090 N500511 789.00 789.50 0.50 0.116 0.085 0.014 0.430 N500512 789.50 790.00 0.50 0.024 0.006 0.002 0.230 N500513 790.00 791.00 1.00 0.022 0.016 0.002 0.130 N500514 791.00 791.50 0.50 0.092 0.065 0.008 0.520 N500515 791.50 792.00 0.50 0.017 0.004 0.001 0.070 N500516 792.00 793.00 1.00 0.022 0.011 0.002 0.120 N500517 793.00 794.00 1.00 0.028 0.021 0.002 0.230 N500519 794.00 795.00 1.00 0.014 0.006 0.001 0.110 N500520 795.00 796.00 1.00 0.036 0.005 0.001 0.160 N500521 796.00 797.00 1.00 0.029 0.005 0.001 0.100 N500522 797.00 798.00 1.00 0.028 0.007 0.001 0.040 N500523 798.00 799.00 1.00 0.018 0.007 0.001 0.070 N500524 799.00 800.00 1.00 0.013 0.006 0.002 0.040 N500525 800.00 801.00 1.00 0.011 0.009 0.001 0.060 N500526 801.00 802.00 1.00 0.011 0.007 0.001 0.020 N500527 802.00 803.00 1.00 0.018 0.012 0.001 0.020 N500528 803.00 804.00 1.00 0.022 0.022 0.003 0.020 Page 17 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500529 804.00 805.00 1.00 0.046 0.067 0.016 0.020 N500531 805.00 806.00 1.00 0.045 0.027 0.003 0.030 N500532 806.00 806.40 0.40 0.116 0.097 0.012 0.040 MINOR INTERVALS: 692.80-707.00 : IGB Gabbro SHARP CONTACT WITH OVERLYING UPPER SERIES GABBRO. MARKED DECREASE IN GRAIN SIZE, TEXTURE AND COMPOSITION, NOW BEING FINE-MEDIUM GRAINED, INTERGRANULAR, AND 50-60% CLINOPYROXENE, 40-50% PLAGIOCLASE AND UP TO 5% BIOTITE. GRADUALLY FRACTIONATES DOWNHOLE BUT GENERALLY VERY HOMOGENOUS. PHENOCRYSTS OF GREEN-BLACK RELICT PYROXENE WHICH HAVE BEEN CHLORITIZED GIVE CORE A SPOTTED APPEARANCE. 1% FINELY DISSEMINATED PY-PO WITH MINOR CPY MINERALIZATION. 707.00-719.40 : IMGB Melagabbro ROCK GRADUALLY FRACTIONATES TO A MORE MAFIC, MELAGABBROIC COMPOSITION. TEXTURE CHANGES FROM DOMINANTLY INTERGRANULAR TO WEAKLY OIKOCRYSTIC WITH PLAGIOCLASE THEN CLINOPYROXENE OIKOCRYSTS ENCLOSING EARLIER PHASES. BIOTITE RICH (UP TO 10% IN SOME LOCATIONS) AND GENERALLY ABSENT OF SULFIDE MINERALIZATION. CHLORITIZED PHENOCRYSTS, WHICH ARE ABUNDANT IN THE OVERLYING GABBRO GRADUALLY DISSAPEAR. CONTACT MARKED ROUGHLY WHERE OLIVINE BEGINS TO COMPRISE >5% OF MODAL COMPOSITION. 719.40-745.40 : IOMGB Olivine Melagabbro SIMILAR IN APPEARANCE TO OVERLYING MELAGABBRO BUT WITH LESS PLAGIOCLASE AND MORE OLIVINE. SEEMS TO FRACTIONATE INWARDS FROM UPPER AND LOWER CONTACTS WITH ROCKS FROM 727.3-731m NEARLY ULTRAMAFIC IN COMPOSITION. 5-20% PLAGIOCLASE, 10-30% OLIVINE 50-60% PYROXENE AND 5% BIOTITE. OLIVINE IS VERY FRESH, NO SERPENTINE ALTERATION NOTED. OCCURS AS CHADACRYSTS WITHIN CLINOPYROXENE OIKOCRYSTS. PLAGIOCLASE OCCURS AS ANHEDRAL INTERSTITIAL GROUNDMASS AND AS LATHS. 745.40-762.80 : IPDT IPDT UNIT CONTACT IS TRANSITIONAL, MARKED BY NEAR ABSENCE OF PLAGIOCLASE. MASSIVE AND FINE GRAINED OVERALL WITH 20-40% OLIVINE, 40-50% CLINOPYROXENE, 0-10% PLAGIOCLASE, AND UP TO 5% BIOTITE. VERY WEAK SERPENTINE ALTERATION GIVE CORE A BLACK STRIPED APPEARANCE. SERPENTINE ALTERATION IS STRONGER AS LOWER CONTACT IS APPROACHED. LOWER CONTACT WITH OLIVINE MELAGABBRO (AS ABOVE), IS MARKED BY ABRUPT LOSS OF SERPENTINE ALTERATION. VEIN CONTROLLED PYRHOTITE MINERALIZATION AT 746.2 AND 747.1m. 762.80-806.40 : IOMGB Olivine Melagabbro REVERSELY FRACTIONATED DOWNHOLE, BECOMING MORE PLAGIOCLASE RICH AND OLIVINE POOR TOWARDS LOWER CONTACT (45-55% CLINOPYROXENE, 10-30% OLIVINE, 10-35% PLAGIOCLASE, 5% BIOTITE). GENERALLY HOMOGENOUS EXCEPT FOR SULFIDE BEARING VARITEXTURED INTERVALS FROM 788.4-791.2m. ISOLATED BLEB OF STRONGLY TARNISHED SULFIDE (YELLOW, BRONZE, BLUE COLOUR). POSSIBLY PO/CPY/BN AT 801.4m. SHARP LOWER CONTACT MARKED BY CHLORITIZED FAULT? BRECCIA. Page 18 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Sample # Minor 692.80-707.00: Chlorite, Spots, Moderate CHLORITIZED PYROXENE PHENOCRYSTS 707.00-712.00: Chlorite, Spots, Weak 721.30-721.30: Chlorite, Fracture Filling, Moderate 738.20-738.80: Chlorite, Fracture Filling, Strong CHLORITIC FRACTURE AT 15 DTCA 745.40-762.80: Serpentinization, Veins, Weak 771.60-771.70: Chlorite, Fracture Filling, Strong 777.70-777.70: Chlorite, Fracture Filling, Strong 798.70-806.40: Chlorite, Veins, Weak BLACK CHLORITIC VEINS HAVE HALOS OF BLACK, MEDIUM GRAINED AMPHIBOLE Minor Mineralization: 692.80-707.00: Pyrrhotite/Pyrite/Chalcopyrite, Disseminated, 1% 746.20-746.20: Pyrrhotite, Veins, 5% 2mm WIDE CARBONATE/CHLORITE VEIN WITH SULFIDE 747.10-747.10: Pyrrhotite, Veins, 5% AS ABOVE, SULFIDE IN CARBONATE/CHLORITE VEIN 779.20-783.70: Pyrrhotite, Disseminated, 1-2% 785.20-786.20: Pyrrhotite/Chalcopyrite, Trace DOMINANTLY PO. VERY F.G AND TYPICALLY FOUND NEAR LATE CHLORITIC FRACTURES 788.40-790.00: Pyrrhotite/Pyrite/Chalcopyrite, Disseminated, 1% UP TO 3% LOCALLY (789.3-789.5). VERY F.G 791.00-791.40: Pyrrhotite/Pyrite/Chalcopyrite, Blebby, 4% F.G AND C.G BLEBS/DISSEMINATED SULFIDE ASSOCIATED WITH VARITEXTURED ZONE. 801.40-801.40: Pyrrhotite/Chalcopyrite, Blebby, 1% SINGLE, M.G. BLEB OF SULFIDE. TARNISHED TO BRONZE/YELLOW/BLUE COLOUR. POSSIBLE BO From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Minor Structure: 721.30-721.30: Slikensides SLICKENLINES WITHIN CHLORITIC FRACTURE 771.60-771.70: Fractured CHLORITIC FRACTURE 777.70-777.70: Fractured CHLORITIC FRACTURE 806.40-806.40: Fault CHLORITIC FAULT GOUGE. MARKS SHARP CONTACT WITH UNDERLYING PERIDOTITE Page 19 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Minor Lithology 692.80-707.00: Fine Grained - Medium Grained 692.80-707.00: Pyroxene Phyric 692.80-707.00: Massive INTERGRANULAR TEXTURE 707.00-719.40: Poikolitic PLAGIOCLASE THEN PYROXENE OIKOCRYSTS ENCLOSE EARLIER PHASES. OIKOCRYSTS ARE MEDIUM GRAINED 707.00-719.40: Fine Grained - Medium Grained 707.00-719.40: Massive 719.40-745.40: Poikolitic PYROXENE OIKOCRYSTS ENCLOSE OLIVINE AND EARLY PYROXENE PHENOCRYSTS 719.40-745.40: Fine Grained 719.40-745.40: Massive 745.40-762.80: Poikolitic MEDIUM GRAINED PYROXENE OIKOCRYSTS ENCLOSE OLIVINE CHADACRYSTS 745.40-762.80: Massive 745.40-762.80: Fine Grained 762.80-806.40: Fine Grained 788.00-788.00: Broken Core BROKEN CHLORITIC CORE 788.40-788.70: Varitextured COARSE GRAINED PODS OF PLAGIOCLASE CARBONATE AND CHLORITE 791.00-791.40: Varitextured COARSE GRAINED PODS OF LEUCOCRATIC GABBRO AS ABOVE. ASSOCIATED WITH SULFIDE MINERALIZATION 806.40 826.60 IUMS, Ultramafic Series Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 20 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500533 806.40 807.00 0.60 0.053 0.016 0.004 0.080 N500533 806.40 807.00 0.60 0.053 0.016 0.004 0.080 N500534 807.00 808.00 1.00 0.093 0.046 0.005 0.020 N500534 807.00 808.00 1.00 0.093 0.046 0.005 0.020 N500535 808.00 809.00 1.00 0.111 0.100 0.021 0.060 N500535 808.00 809.00 1.00 0.111 0.100 0.021 0.060 N500536 809.00 810.00 1.00 0.059 0.047 0.016 0.230 N500536 809.00 810.00 1.00 0.059 0.047 0.016 0.230 N500537 810.00 811.00 1.00 0.103 0.082 0.011 0.120 N500537 810.00 811.00 1.00 0.103 0.082 0.011 0.120 N500538 811.00 812.00 1.00 0.380 0.273 0.033 0.930 N500539 812.00 813.00 1.00 0.548 0.402 0.061 0.860 N500540 812.00 813.00 1.00 0.507 0.378 0.061 N500541 813.00 814.00 1.00 0.166 0.100 0.023 0.400 N500542 814.00 815.00 1.00 0.157 0.109 0.017 0.310 N500543 815.00 816.00 1.00 0.237 0.129 0.007 0.450 N500544 816.00 817.00 1.00 0.550 0.426 0.057 0.570 N500545 817.00 818.00 1.00 0.249 0.206 0.032 1.230 N500546 818.00 819.00 1.00 0.303 0.213 0.025 0.280 N500547 819.00 820.00 1.00 0.187 0.070 0.021 0.530 N500548 820.00 821.00 1.00 0.052 0.029 0.021 0.220 N500549 821.00 822.00 1.00 0.080 0.050 0.017 0.420 N500551 822.00 823.00 1.00 0.075 0.051 0.009 0.440 N500552 823.00 824.00 1.00 0.685 0.266 0.034 0.350 N500553 824.00 825.00 1.00 0.233 0.137 0.030 0.280 N500554 825.00 826.00 1.00 0.779 0.518 0.045 0.660 N500539 812.00 813.00 1.00 0.548 0.402 0.061 0.860 N500540 812.00 813.00 1.00 0.507 0.378 0.061 N500541 813.00 814.00 1.00 0.166 0.100 0.023 0.400 N500542 814.00 815.00 1.00 0.157 0.109 0.017 0.310 N500543 815.00 816.00 1.00 0.237 0.129 0.007 0.450 N500544 816.00 817.00 1.00 0.550 0.426 0.057 0.570 N500545 817.00 818.00 1.00 0.249 0.206 0.032 1.230 N500546 818.00 819.00 1.00 0.303 0.213 0.025 0.280 N500547 819.00 820.00 1.00 0.187 0.070 0.021 0.530 N500548 820.00 821.00 1.00 0.052 0.029 0.021 0.220 N500549 821.00 822.00 1.00 0.080 0.050 0.017 0.420 N500551 822.00 823.00 1.00 0.075 0.051 0.009 0.440 N500552 823.00 824.00 1.00 0.685 0.266 0.034 0.350 N500553 824.00 825.00 1.00 0.233 0.137 0.030 0.280 N500554 825.00 826.00 1.00 0.779 0.518 0.045 0.660 Page 21 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology MINOR INTERVALS: 806.40-811.80 : IOMGNO Olivine Melagabbrono STRONGLY SERPENTINIZED MELAGABBRO, MARKEDLY COARSER THAN OVERLYING UNIT. STRONGLY OIKOCRYSTIC, WITH COARSE CLINO AND ORTHOPYROXENE ENCLOSING OLIVINE CHADACRYSTS. PLAGIOCLASE OCCURS AS AN INTERCUMULUS PHASE BETWEEN PYROXENE AND OLIVINE. 50-65% PYROXENE (ORTHO+CLINO), 20-35% OLIVINE (SERPENTINIZED), 10-20% PLAGIOCLASE, 10% BIOTITE. HAS A SHEARED APPEARANCE FROM 806.4-809.2m DUE TO FINE SERPENTINE VEINS. BLEBBY INTERSTITIAL SULFIDE FROM 810.1-811.8m IS CLEARLY INTERCUMULUS AND IS DOMINANTLY PO WITH MINOR CPY. 811.80-826.60 : IPDT IPDT STRONGLY SERPENTINIZED PERIDOTITE. CONTACT MARKED BY ABSENCE OF INTERCUMULUS PLAGIOCLASE. PYROXENE AND OLIVINE ARE STRONGLY SERPENTINIZED AND FORM A MEDIUM-COARSE GRAINED ADCUMULATE TEXTURE. PYROXENE FORM OIKOCRYSTS ENCLOSING FINER GRAINED OLIVINE. CARBONATE VEINING SOMETIMES ASSOCIATED WITH SERPENTINE. 5% INTERCUMULUS PO+PY MINERALIZATION FROM 811.8-813m Minor 806.40-811.80: Carbonate, Veins, Weak CARBONATE ASSOCIATED WITH SOME SERPENTINE VEINS 806.40-811.80: Serpentinization, Veins, Moderate 811.80-826.60: Carbonate, Veins, Weak ASSOCIATED WITH SOME SERPENTINE VEINS 811.80-826.60: Serpentinization, Pervasive, Moderate PERVASSIVE TO VEIN CONTROLLED SERPENTINE ALTERATION Minor Mineralization: 810.10-811.80: Pyrrhotite/Chalcopyrite, Intercumulus, 2% DOMINANTLY PO 811.80-813.00: Pyrrhotite/Pyrite, Intercumulus, 8% IRREGULAR BLEBS/BLOCKS OF IRON SULFIDE THROUGHOUT 813.00-815.20: Pyrrhotite/Pyrite, Disseminated, 2% 815.20-815.50: Pyrrhotite/Pyrite, Disseminated, 5% DISSEMINATED TO BLEBBY HABIT 815.50-816.40: Pyrrhotite/Pyrite, Disseminated, 1% TRACE TO 1% 816.40-818.00: Pyrrhotite/Pyrite, Disseminated, 2-4% FINELY DISSEMINATED SULFIDE AS WELL AS NARROW CARBONATE/PYRRHOTITE VEINS 818.00-820.00: Pyrrhotite/Pyrite, Trace, TRACE% SPARSE, VERY FINE GRAINED SULFIDE THROUGHOUT 821.90-825.00: Pyrrhotite/Pyrite, Disseminated, 2% VERY FINE GRAINED SULFIDE 825.00-826.60: Pyrrhotite/Pyrite/Chalcopyrite, Disseminated, 3% DOMINANTLY IRON SULFIDE WITH MINOR CPY Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 22 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology Minor Structure: 806.40-811.80: Veins SERPENTINE VEINS 811.80-826.60: Veins SERPENTINE VEINS Minor 806.40-807.00: Broken Core 806.40-811.80: Medium Grained - Coarse Grained COARSE GRAINED OIKOCRYSTS WITH FINER INTERSTITIAL PLAGIOCLAS. 806.40-811.80: Mesocumulate CUMULATE PYROXENE + OLIVINE 809.10-809.20: Coarse Grained COARSE GRAINED LEUCOCRATIC POD 811.80-826.60: Oikocrysts PYROXENE ENCLOSES OLIVINE AND PYROXENE CHADACRYSTS 811.80-826.60: Adcumulate PYROXENE AND OLIVINE ARE CUMULATE PHASES 811.80-826.60: Medium Grained - Coarse Grained 821.00-821.30: Broken Core Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 826.60 835.90 IGLS, Lower Series Gabbro N500556 827.00 828.00 1.00 0.722 0.393 0.074 0.770 N500556 827.00 828.00 1.00 0.722 0.393 0.074 0.770 N500557 828.00 829.00 1.00 0.658 0.428 0.057 0.880 N500557 828.00 829.00 1.00 0.658 0.428 0.057 0.880 N500558 829.00 830.00 1.00 1.290 0.703 0.093 1.210 N500558 829.00 830.00 1.00 1.290 0.703 0.093 1.210 N500559 830.00 831.00 1.00 0.830 0.466 0.059 0.870 N500559 830.00 831.00 1.00 0.830 0.466 0.059 0.870 N500560 831.00 832.00 1.00 1.510 0.918 0.101 0.870 N500560 831.00 832.00 1.00 1.510 0.918 0.101 0.870 N500561 832.00 833.00 1.00 1.970 1.515 0.092 1.470 N500562 833.00 833.40 0.40 2.290 1.305 0.165 N500563 833.40 834.00 0.60 2.330 1.280 0.140 1.130 N500565 834.00 835.00 1.00 2.120 1.210 0.138 1.290 N500566 835.00 835.90 0.90 1.925 1.010 0.146 1.040 N500562 833.00 833.40 0.40 2.290 1.305 0.165 N500563 833.40 834.00 0.60 2.330 1.280 0.140 1.130 N500565 834.00 835.00 1.00 2.120 1.210 0.138 1.290 N500566 835.00 835.90 0.90 1.925 1.010 0.146 1.040 Page 23 of 27 Feb 13, 2015

Hole Number: SL-14-006 From Mineralization: To Lithology 826.60-827.00: Pyrrhotite/Chalcopyrite, Blebby, 5% BLEBBY AND VEIN CONTROLLED SULFIDE. BLEBS ARE WITHIN COARSE LEUCOCRATIC FRAGMENTS THAT LOOK LIKE XENOLITHS. FINELY DISSEMINATED SULFIDE HERE IS DOMINANTLY PO. 827.00-827.40: MINOR INTERVALS: 826.60-832.60 : IPXT IPXT MINERALIZED MELAGABBRO TO PYROXENITE. SHARP CONTACT WITH OVERLYING PERIDOTITE MARKED BY VARITEXTURED ZONE THAT APPEARS TO BE A STRONGLY ALTERED MIXING ZONE. COARSE GRAINED LEUCOCRATIC PODS/VEINS ARE FOUND THROUGHOUT AND CAN BE ASSOCIATED WITH SULFIDE MINERALIZATION. 1-10% SULFIDE AS INDICATED IN THE MINERALIZATION LOG, IS COMPRISED OF BLEBBY, DISSEMINATED AND VEIN HOSTED PO+PY+CPY. 832.60-835.90 : IMGNO Melagabbronorite SULFIDE RICH VARITEXTURED ZONE DEFINES CONTACT BETWEEN OVERLYING PYROXENITE AND THIS PLAGIOCLASE BEARING MELAGABBRONORITE. UP TO 20% PO-CPY-PY WITHIN THIS VARITEXTURED ZONE FROM 832.6-833.2m. SULFIDE APPEARS TO BE DOMINANTLY WITHIN XENOLITHS (AUTOLITHS). UNIT GRADUALLY FINES AS THE DIFFUSE CONTACT WITH THE FOOTWALL SEDIMENTS IS APPROACHED. DISSEMINATED CPY-PO-PY MINERALIZATION HAS AN INTERCUMULUS HABIT. FINE-MEDIUM GRAINED ADCUMULATE PYROXENE DOMINATE THE SILICATE MINERALOGY. Minor Mineralization: 826.60-827.00: Pyrrhotite/Pyrite/Chalcopyrite, Blebby, 5% BLEBBY AND VEIN CONTROLLED SULFIDE. BLEBS ARE WITHIN COARSE LEUCOCRATIC FRAGME 827.00-832.60: Pyrrhotite/Pyrite, Disseminated, 2-4% FINE GRAINED DISSEMINATED IRON SULFIDE THROUGHOUT INTERVAL. 828.60-828.70: Pyrrhotite/Chalcopyrite, Blebby, 5% BLEBBY CPY RICH SULFIDE IN PEGMATITIC POD 829.40-830.60: Chalcopyrite, Blebby, 1% CPY CONFINED TO BLEBS WITHIN LEUCOCRATIC PODS/XENOLITHS 832.40-832.50: Pyrrhotite/Chalcopyrite, Veins, 10% PYRRHOTITE RICH VEIN WITH BLEBBY CPY RICH SULFIDE ADJACENT 832.60-833.20: Pyrrhotite/Pyrite/Chalcopyrite, Blebby, 3% FINE TO MEDIUM GRAINED BLEBS. 60-40 PO-CPY RATIO 833.20-833.30: Pyrrhotite/Chalcopyrite, Fragments, 20% SULFIDE RICH AUTOLITH? 833.20-835.90: Pyrrhotite/Pyrite/Chalcopyrite, Disseminated, 5% FINELY DISSEMINATED SULFIDE THROUGH TO LOWER CONTACT Minor Structure: 832.40-832.40: Veins SULFIDE VEIN Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 24 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Minor Lithology 826.60-827.00: Varitextured SULFIDIC MIXING ZONE BETWEEN PERIDOTITE AND PYROXENITE. 827.00-829.40: Fine Grained GENERALLY FINE GRAINED WITH SMALL ZONES OF COARSER PYROXENITE AS INDICATED BELOW 828.60-828.70: Pegmatitic PEGMATITIC POD OF LEUCOCRATIC GABBRO 829.40-831.00: Medium Grained MOTTLED ZONE WITH VARIABLE GRAINSIZES 832.60-833.20: Varitextured XENOLITHS/PODS OF C.G LEUCOCRATIC GABBRO AND SULFIDIC GABBRO 833.20-835.90: Adcumulate PYROXENE CUMULATE WITH INTERSTITAL SULFIDE AND PLAGIOCLASE 833.20-835.90: Medium Grained - Fine Grained GRADUALLY FINES TO FINE GRAINED AT CONTACT 835.90 863.00 MQZT, Mafic metasediment Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 25 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology HORNFELSED QUETICO SEDIMENTS HAVE A GREY COLOUR AND DOMINANTLY FINE GRAINED MASSIVE TEXTURE TO 855.5m. CORE HAS A WHITE SPOTTED TEXTURE POSSIBLY DUE TO RECRYSTALIZATION OF FELDSPAR/QUARTZ? FOOTWALL CPY-PO MINERALIZATION FOUND FROM 838-840m. MINERALIZATION CONSISTS OF VERY FINE FRACTURES OF CPY-PO AND BLEBBY PO WITHIN LEUCOCRATIC VEINS. VEIN/LEUCOSOME HOSTED PY MINERALIZATION FROM 854m TO EOH. Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500567 835.90 837.00 1.10 0.116 0.071 0.016 0.260 N500568 837.00 838.00 1.00 0.047 0.026 0.001 0.170 N500569 838.00 838.50 0.50 0.024 0.010 0.002 0.180 N500571 838.50 839.00 0.50 1.195 0.909 0.068 0.890 N500572 839.00 840.00 1.00 0.223 0.130 0.029 N500573 840.00 841.00 1.00 0.005 0.002 0.001 N500574 841.00 842.00 1.00 0.005 0.002 0.001 N500575 842.00 843.00 1.00 0.005 0.001 0.001 N500576 843.00 844.00 1.00 0.005 0.001 0.001 N500577 844.00 845.00 1.00 0.005 0.001 0.001 0.240 N500578 845.00 846.00 1.00 0.005 0.002 0.001 N500579 846.00 847.00 1.00 0.005 0.001 0.001 N500580 846.00 847.00 1.00 0.005 0.001 0.001 N500581 847.00 848.00 1.00 0.005 0.002 0.001 N500582 848.00 849.00 1.00 0.005 0.001 0.001 N500583 849.00 850.00 1.00 0.005 0.002 0.001 0.270 N500584 850.00 851.00 1.00 0.005 0.001 0.001 N500585 851.00 852.00 1.00 0.005 0.001 0.001 N500586 852.00 853.00 1.00 0.005 0.002 0.001 N500587 853.00 854.00 1.00 0.005 0.001 0.001 N500588 854.00 855.00 1.00 0.005 0.001 0.001 0.280 N500589 855.00 856.00 1.00 0.005 0.002 0.001 N500591 856.00 857.00 1.00 0.005 0.002 0.001 N500592 857.00 858.00 1.00 0.005 0.003 0.001 N500593 858.00 859.00 1.00 0.005 0.002 0.001 N500594 859.00 860.00 1.00 0.005 0.001 0.001 0.270 N500595 860.00 861.00 1.00 0.005 0.020 0.003 N500596 861.00 862.00 1.00 0.005 0.002 0.001 N500597 862.00 863.00 1.00 0.005 0.002 0.001 N500720 862.00 863.00 1.00 790.000 88.000 131.000 0.023 0.011 0.001 0.500 855.50-863.00: Chlorite, Veins, Moderate CHLORITE FOUND WITHIN LEUCOCRATIC BANDS Mineralization: 838.00-840.00: Pyrrhotite/Chalcopyrite, Veins, 1% LOCALLY UP TO 3%. CPY RICH SULFIDE IS CONFINED TO FRACTURES OR LEUCOCRATIC VEINS/PODS CUTTING SEDIMENT 855.00-863.00: Pyrite, Veins, 3% PYRITE WITHIN LEUCOSOME OF SEDIMENT. APPEARS PRIMARY Structure: 855.00-863.00: Banded QUARTZ RICH BANDS Page 26 of 27 Feb 13, 2015

Hole Number: SL-14-006 From To Lithology 835.90-855.00: Hornfelsed BLEACHED GREY COLOUR. ORIGINAL BEDDING NOT OBSERVED. SPOTTED APPEARANCE. 855.00-863.00: Banded WEAK BANDING DEFINED BY QUARTZ RICH LEUCOSOME Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Survey Data Depth Azimuth Decimal Dip Decimal Test Type Flag 0.00 270.00-85.00 REFLEX O 92.00 261.90-82.40 REFLEX O 122.00 298.00-82.00 REFLEX N 152.00 276.00-81.00 REFLEX O 182.00 271.60-80.00 REFLEX O 212.00 273.30-79.00 REFLEX O 242.00 280.50-78.30 REFLEX O 272.00 275.50-77.70 REFLEX O 302.00 284.40-77.30 REFLEX O 332.00 288.50-76.40 REFLEX O 362.00 291.10-75.60 REFLEX O 392.00 295.50-74.80 REFLEX O 422.00 295.40-74.20 REFLEX O 452.00 290.50-73.40 REFLEX O 482.00 293.50-72.70 REFLEX O 512.00 295.70-72.00 REFLEX O 542.00 289.70-71.50 REFLEX O 572.00 276.90-70.90 REFLEX O 602.00 292.80-70.70 REFLEX O 632.00 294.50-69.80 REFLEX O 662.00 290.90-69.00 REFLEX O 692.00 296.80-68.50 REFLEX O 722.00 301.30-67.80 REFLEX O 752.00 301.70-67.90 REFLEX O 782.00 302.10-66.50 REFLEX O 812.00 307.00-65.60 REFLEX O 842.00 304.10-65.20 REFLEX O Comments Page 27 of 27 Feb 13, 2015

Hole Number SL-14-007 Project Name: Project Code: Location: Start Date: Completed Date: Contractor: Core Storage: Units: Comments: Detailed Lithology From To Project SUNDAY LAKE 23 Dec 01, 2014 Dec 11, 2014 Orbit Garant TMC Core Shack METRIC Coordinates Primary Coordinates Grid: UTM83-16 North: 5,395,240.00 East: 334,330.00 Elev: 488.00 Destination Coordinates Grid: LL83 North: East: Elev: 48.69-89.25 488.00 TESTING SW OF SL-13-002 ALONG POSSIBLE STRUCTURAL LINEAMENT THROUGH SUNDAY LAKE. Lithology 0.00 14.30 CAS, CASING AND OVERBURDEN 14.30 20.10 MQZT, Mafic metasediment QUETICO METASEDIMENTS. ANNEALED FRACTURES WITH HEMATITE, CHLORITE, CARBONATE AND MINOR EPIDOTE ALTERATION. BROKEN CORE AS INDICATED IN TEXTURE LOG. 14.30-20.10: Epidote, Fracture Filling, Moderate 14.30-20.10: Carbonate, Fracture Filling, Weak MOST FRACTURES CONTAIN CARBONATE 14.30-20.10: Hematite, Pervasive, Moderate PREFERRENTIALLY ALTERS LEUCOCRATIC BANDS AND EXTENDS FROM FRACTURE ZONES 14.30-20.10: Hematite, Fracture Filling, Moderate NARROW 1-5mm ANNEALED FRACTURES Structure: 14.30-20.10: Banded 14.30-20.10: Fractured 14.30-20.10: Banded 16.80-17.10: Broken Core 18.10-18.30: Broken Core 20.10 24.40 IGRD, Granodiorite Sample # Collar Dip: Length: Hole Size: Hole Type: Casing: Collar Survey: N Multishot Survey: N Collar -78.00 Collar Az: 295.00 497.00 NQ DD Left in Hole Plugged: N Pulse EM Survey: N From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 1 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology STRONGLY FOLIATED GRANODIORITE. CONTACTS WITH SEDIMENTS ARE BANDED AND THIS UNIT COULD BE THE LEUCOSOME OF THE GNEISS. MODERATELY HEMATIZED IS PERVASSIVE BUT STRONGER ALONG FRACTURES. 20.10-24.40: Epidote, Fracture Filling, Weak 20.10-24.40: Carbonate, Fracture Filling, Weak 20.10-24.40: Hematite, Pervasive, Moderate PREFERRENTIALLY ALTERS LEUCOCRATIC BANDS AND EXTENDS FROM FRACTURE ZONES 20.10-24.40: Hematite, Fracture Filling, Moderate NARROW 1-5mm ANNEALED FRACTURES Structure: 20.10-24.40: Foliation 20.10-24.40: Foliated 20.10-24.40: Coarse Grained Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 24.40 39.60 MQZT, Mafic metasediment QUETICO METASEDIMENTS. STRONGLY FRACTURED THROUGHOUT WITH LATE BRITTLE FRACTURES AND ANNEALED FRACTURES THAT CONCENTRATE ALTERATION. 24.40-39.60: Epidote, Fracture Filling, Weak 24.40-39.60: Carbonate, Fracture Filling, Weak MOST FRACTURES CONTAIN CARBONATE 24.40-39.60: Hematite, Pervasive, Weak PERVASSIVE ALTERATION IS ADJACENT TO FRACTURES 24.40-39.60: Hematite, Fracture Filling, Moderate NARROW 1-5mm ANNEALED FRACTURES Mineralization: 24.40-39.60: Pyrite, Fracture Filling, 3% Structure: 24.40-39.60: Banded 24.40-39.60: Fractured 24.40-39.60: Banded 34.10-34.80: Broken Core 39.60 40.20 IGRD, Granodiorite PINK GRANODIORITE. STRONGLY FRACTURED WITH PEGMATITIC QUARTZ. MODERATE HEMATITE AND CHLORITE ALTERATION. Page 2 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology 39.60-40.20: Hematite, Pervasive, Moderate PREFERRENTIALLY ALTERS LEUCOCRATIC BANDS AND EXTENDS FROM FRACTURE ZONES 39.60-40.20: Hematite, Fracture Filling, Moderate NARROW 1-5mm ANNEALED FRACTURES 39.60-40.20: Chlorite, Fracture Filling, Moderate 39.60-40.20: Carbonate, Fracture Filling, Weak MOST FRACTURES CONTAIN CARBONATE 39.60-40.20: Pegmatitic 39.60-40.20: Foliated 39.60-40.20: Coarse Grained Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 40.20 40.90 MQZT, Mafic metasediment 40.20-40.90: Carbonate, Fracture Filling, Weak MOST FRACTURES CONTAIN CARBONATE 40.20-40.90: Hematite, Pervasive, Weak 40.20-40.90: Hematite, Fracture Filling, Moderate NARROW 1-5mm ANNEALED FRACTURES Structure: 40.20-40.90: Banded 40.20-40.90: Medium Grained 40.20-40.90: Banded 40.90 43.00 IGRD, Granodiorite PINK GRANODIORITE WITH ABUNDANT PEGMAITITC QUARTZ. VERY FRACTURED WITH MODERATE CHLORITE, HEMATITE, EPIDOTE AND SERICITE ALTERATION. 40.90-43.00: Sericite, Fracture Filling, Moderate 40.90-43.00: Hematite, Pervasive, Moderate PREFERRENTIALLY ALTERS LEUCOCRATIC BANDS AND EXTENDS FROM FRACTURE ZONES 40.90-43.00: Hematite, Fracture Filling, Moderate NARROW 1-5mm ANNEALED FRACTURES 40.90-43.00: Epidote, Fracture Filling, Moderate 40.90-43.00: Chlorite, Fracture Filling, Moderate Page 3 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 40.90-43.00: Fractured 40.90-43.00: Pegmatitic 40.90-43.00: Foliated 43.00 44.50 MQZT, Mafic metasediment QUETICO METASEDIMENTS. BOUDINAGED GRANODIORITE WITHIN INTERVAL. NOT ALTERED. Structure: 43.00-44.50: Banded 43.00-44.50: Medium Grained 43.00-44.50: Banded 44.50 45.90 IGRD, Granodiorite WHITE GRANODIORITE. ONLY VERY WEAK HEMATITE ALTERATION ALONG FRACTURES. WEAK CHLORITE ALTERATION WITHIN PEGMATITE ZONES. 44.50-45.90: Chlorite, Patchy, Weak 44.50-45.90: Hematite, Fracture Filling, Weak Structure: 44.50-45.90: Foliation 44.50-45.90: Coarse Grained 44.70-44.90: Pegmatitic 45.90 53.50 MQZT, Mafic metasediment QUETICO METASEDIMENTS. ALTERATION CONFINED TO FRACTURES, WITH SMALL ZONES OF STRONG PERVASSIVE HEMATITE ALTERATION 52.2-53.5m. 45.90-53.50: Epidote, Fracture Filling, Weak 45.90-53.50: Hematite, Fracture Filling, Moderate NARROW 1-5mm ANNEALED FRACTURES 52.20-53.50: Hematite, Pervasive, Strong PREFERRENTIALLY ALTERS LEUCOCRATIC BANDS AND EXTENDS FROM FRACTURE ZONES Structure: 45.90-53.50: Banded Page 4 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 45.90-53.50: Banded 52.00-53.50: Fractured 52.50-52.60: Brecciated 53.50 57.30 IGRD, Granodiorite PINK TO RED GRANODIORITE. AS ABOVE, CONTACTS ARE BAND PARALLEL. PERVASSIVE HEMATITE ALTERATION WITH STRONG HEMATITE/CHLORITE ALTERATION ALONG FRACTURES. 53.50-57.30: Chlorite, Fracture Filling, Moderate 53.50-57.30: Hematite, Pervasive, Moderate 53.50-57.30: Hematite, Fracture Filling, Strong NARROW 1-5mm ANNEALED FRACTURES Structure: 53.50-57.30: Foliation 53.50-57.30: Fractured ANNEALED FRACTURES, NEARLY BRECCIATED 53.50-57.30: Foliated 53.50-57.30: Coarse Grained 57.30 58.70 MQZT, Mafic metasediment QUETICO METASEDIMENTS. 57.30-58.70: Carbonate, Fracture Filling, Weak 57.30-58.70: Hematite, Fracture Filling, Moderate NARROW 1-5mm ANNEALED FRACTURES 58.00-58.70: Chlorite, Fracture Filling, Moderate 58.00-58.70: Hematite, Pervasive, Strong STRONGER ALTERATION IN FRACTURED ZONE Structure: 57.30-58.70: Banded 57.30-58.70: Medium Grained 57.30-58.70: Banded 58.00-58.70: Broken Core 58.00-58.70: Fractured 58.70 59.30 IGRD, Granodiorite Page 5 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology NARROW BAND OF GRANODIORITE. MODERATELY HEMATIZED. Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 58.70-59.30: Chlorite, Fracture Filling, Moderate 58.70-59.30: Hematite, Pervasive, Moderate 58.70-59.30: Foliated 59.30 63.80 MQZT, Mafic metasediment 63.80 66.40 IGRD, Granodiorite PINK GRANODIORITE. STRONGLY FOLIATED WITH MINOR FRACTURE CONTROLLED HEMATITE/CARBONATE/CHLORITE ALTERATION. MINOR BANDS OF SEDIMENT WITHIN INTERVAL. 63.80-66.40: Carbonate, Fracture Filling, Weak 63.80-66.40: Chlorite, Fracture Filling, Moderate 63.80-66.40: Hematite, Fracture Filling, Strong 63.80-66.40: Hematite, Pervasive, Moderate Structure: 63.80-66.40: Foliation 63.80-66.40: Medium Grained 63.80-66.40: Foliated 63.80-66.40: Banded 66.40 67.10 MQZT, Mafic metasediment BAND OF STONGLY GNEISSIC QUETICO SEDIMENTS BETWEEEN GRANODIORITE BANDS. 66.40-67.10: Hematite, Fracture Filling, Weak Mineralization: 66.40-67.10: Pyrite, Fracture Filling, 1% Structure: 66.40-67.10: Banded 66.40-67.10: Medium Grained 66.40-67.10: Banded 67.10 68.20 IGRD, Granodiorite Page 6 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology PINK GRANODIORITE. MODERATE PERVASSIVE HEMATITE ALTERATION. FRACTURE FILLING CARBONATE ALTERATION ALONG HEMATITE/CHLORITE FRACTURES. 67.10-68.20: Hematite, Fracture Filling, Strong 67.10-68.20: Chlorite, Fracture Filling, Weak 67.10-68.20: Carbonate, Fracture Filling, Weak 67.10-68.20: Hematite, Pervasive, Moderate Structure: 67.10-68.20: Foliation 67.10-68.20: Foliated 67.10-68.20: Medium Grained 68.00-68.20: Broken Core Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 68.20 71.30 MQZT, Mafic metasediment STRONGLY BANDED QUETICO SEDIMENTS. HEMATITE ALTERATION STRONGEST ALONG LEUCOCRATIC BANDS AND LATE FRACTUTRES. 68.20-71.30: Epidote, Fracture Filling, Weak 68.20-71.30: Chlorite, Fracture Filling, Moderate 68.20-71.30: Hematite, Fracture Filling, Strong 68.20-71.30: Hematite, Pervasive, Weak Mineralization: 68.20-71.30: Pyrite, Fracture Filling, 1% Structure: 68.20-71.30: Banded 68.20-71.30: Banded 68.90-69.00: Broken Core 69.20-71.30: Medium Grained 71.30 73.90 IGRD, Granodiorite INTERBANDED GRANODIORITE AND METASEDIMENTS. STRONGLY FOLIATED. PERVASSIVE HEMATITE ALTERATION WITH STRONGER ALTERATION ALONG FRACTURES. FAIRLY FRACTURED THROUGHOUT. NARROW FRACTURES WITH BLEACHED HALOS BECOME PROMINENT. 71.30-73.90: Hematite, Fracture Filling, Strong 71.30-73.90: Hematite, Pervasive, Moderate Structure: 71.30-73.90: Foliation Page 7 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology 71.30-73.90: Medium Grained 71.30-73.90: Banded Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 73.90 77.40 MQZT, Mafic metasediment STRONGLY GNEISSIC, BOUDINAGED QUETICO METASEDIMENTS. ALTERATION MOSTLY CONFINED TO FRACTURES AND LEUCOCRATIC BANDS. 73.90-77.40: Chlorite, Fracture Filling, Weak 73.90-77.40: Hematite, Fracture Filling, Moderate Structure: 73.90-77.40: Boundinage 73.90-77.40: Medium Grained 73.90-77.40: Banded 77.40 78.10 IGRD, Granodiorite BAND OF PINK, HEMATIZED GRANODIORITE. FAIRLY COMPETENT RELATIVE TO OTHER INTERVALS. 77.40-78.10: Hematite, Pervasive, Moderate Structure: 77.40-78.10: Foliation 77.40-78.10: Banded 77.40-78.10: Medium Grained 78.10 79.40 MQZT, Mafic metasediment QUETICO METASEDIMENTS. HEMATITE ALTERATION CONFINED TO FRACTURES. FAIRLY COMPETENT CORE RELATIVE TO OVERLYING INTERVALS. 78.10-79.40: Chlorite, Fracture Filling, Moderate 78.10-79.40: Hematite, Fracture Filling, Moderate Mineralization: 78.10-79.40: Pyrite, Fracture Filling, 1% 78.10-79.40: Banded 78.10-79.40: Medium Grained 79.40 83.00 IGRD, Granodiorite Page 8 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology PINK TO RED GRANODIORITE. WEAK FELDSPAR PORPHYRITIC TEXTURE (PORPHYROBLASTIC?). NARROW BRECCIA ZONE IS STRONGLY HEMATIZED WITH A CHLORITIC MATRIX FROM 81.2-81.4m. 79.40-83.00: Chlorite, Fracture Filling, Strong CHLORITIC CORE TO FRACTURES 79.40-83.00: Hematite, Fracture Filling, Strong 79.40-83.00: Hematite, Pervasive, Moderate Mineralization: 79.40-83.00: Pyrite, Fracture Filling, 1% Structure: 79.40-83.00: Foliation 79.40-81.60: Fractured 79.40-83.00: Medium Grained - Coarse Grained 79.40-83.00: Porphyritic FELDSPAR PHYRIC 81.20-81.40: Brecciated Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 83.00 90.00 MQZT, Mafic metasediment DOMINANTLY QUETICO METASEDIMENTS WITH NARROW (<1m) BANDS OF GRANODIORITE. STRONGLY FRACTURED WITH HEMATITE/CARBONATE/CHLORITE/EPIDOTE ALTERATION. 83.00-90.00: Chlorite, Fracture Filling, Moderate 83.00-90.00: Epidote, Fracture Filling, Weak 83.00-90.00: Hematite, Fracture Filling, Strong Structure: 83.00-90.00: Banded 83.00-90.00: Medium Grained 83.00-90.00: Gneissic 90.00 95.20 IGRD, Granodiorite PINK-RED GRANODIORITE. MODERATE PERVASSIVE ALTERATION, WITH VERY STRONG HEMATITE ALTERATION ALONG FRACTURES. CORES OF FRACTURES ARE DOMINANTLY CARBONATE. STRONGLY FRACTURED THROUGHOUT INTERVAL. 90.00-95.20: Carbonate, Fracture Filling, Moderate 90.00-95.20: Hematite, Fracture Filling, Strong 90.00-95.20: Hematite, Pervasive, Moderate Structure: 90.00-95.20: Banded Page 9 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology 90.00-95.20: Foliated 90.00-95.20: Medium Grained 90.00-95.20: Fractured Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 95.20 184.30 MQZT, Mafic metasediment STRONGLY GNEISSIC QUETICO SEDIMENTS. LEUCOCRATIC BANDS ARE <10cm WIDE. PERVASIVE AND FRACTURE CONTROLLED HEMATITE ALTERATION FROM 95.2-128.2m. CARBONATE, CHLORITE AND OR EPIDOTE CAN FILL CORE OF FRACTURES. FROM 115-125m FRACTURES BEGIN TO COALESCE TO FORM DISCREET BRECCIA ZONES AS INDICATED IN TEXTURE LOG. AFTER 128.2m FRACTURES DECREASE AND ONLY MINOR PERVASSIVE HEMATITE ALTERATION IS OBSERVED ADJACENT TO FRACTURES. 95.20-125.00: Chlorite, Fracture Filling, Strong 95.20-130.20: Hematite, Pervasive, Moderate PERVASSIVE ALTERATION WHERE FRACTURING IS STRONG. 95.20-149.50: Epidote, Fracture Filling, Weak 95.20-149.50: Hematite, Fracture Filling, Strong 95.20-184.30: Carbonate, Fracture Filling, Moderate 125.00-184.30: Chlorite, Fracture Filling, Weak 144.20-144.30: Hematite, Fracture Filling, Strong BRECCIA ZONE 176.40-179.40: Chlorite, Pervasive, Strong CHLORITIC UNIT 176.40-179.40: Hematite, Pervasive, Moderate Mineralization: 95.20-122.30: Pyrite, Fracture Filling, 1% 122.30-123.10: Pyrite, Breccia, 5% 123.10-184.30: Pyrite, Fracture Filling, 1% 176.30-176.40: Pyrite, Fracture Filling, 50% 5cm WIDE MASSIVE PYRITE VEIN Structure: 95.20-184.30: Banded Page 10 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology 95.20-184.30: Fractured 95.20-184.30: Medium Grained 95.20-184.30: Gneissic 101.00-101.10: Brecciated 115.00-115.80: Broken Core 115.00-116.10: Brecciated 117.00-118.50: Broken Core 117.00-120.40: Brecciated 122.30-123.10: Brecciated 144.20-144.30: Brecciated 145.70-145.80: Brecciated 147.50-147.60: Brecciated Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 184.30 186.50 IGRD, Granodiorite PINK-RED GRANODIORITE BAND. NARROW FRACTURES WITH BLEACHED HALOS CUT UNIT. 184.30-186.50: Epidote, Spots, Weak 184.30-186.50: Chlorite, Fracture Filling, Moderate 184.30-186.50: Hematite, Pervasive, Moderate Mineralization: 184.30-186.50: Pyrite, Fracture Filling, 3% Structure: 184.30-186.50: Foliation 184.30-186.50: Foliated 184.30-186.50: Medium Grained 186.10-186.30: Brecciated 186.50 235.60 MQZT, Mafic metasediment STRONGLY GNEISSIC QUETICO SEDIMENTS. LEUCOCRATIC BANDS ARE <10cm WIDE. WEAK FRACTURE CONTROLLED HEMATITE ALTERATION TO 194m THEN LARGELY UNALTERED UNTIL 206.7m WHERE A NARROW BRECCIA ZONE IS WEAKLY HEMATIZED. FROM 206.7-237m HEMATITE ALTERATION IS CONFINED TO FRACTURES AGAIN, WITH CHLORITIC CORES TO THE FRACTURES. FROM 209m-237m GNEISSIC BANDING IS LESS APARENT, APPEARING MORE MASSIVE/BEDDED IN TEXTURE. Page 11 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology 186.50-194.00: Hematite, Fracture Filling, Weak 186.50-235.60: Chlorite, Fracture Filling, Weak 186.50-235.60: Carbonate, Fracture Filling, Weak 206.80-215.00: Hematite, Fracture Filling, Weak 215.00-215.60: Hematite, Pervasive, Strong STRONGLY FRACTURED AND ALTERED ZONE 215.60-235.60: Hematite, Fracture Filling, Weak HEMATITE CONFINED TO NARROW FRACTURES AND LEUCOCRATIC BANDS Mineralization: 186.50-202.30: Pyrite, Fracture Filling, 1% 204.30-204.90: Pyrite, Fracture Filling, 5% 204.90-235.60: Pyrite, Fracture Filling, 1% Structure: 186.50-235.60: Foliation 186.50-194.00: Fractured NARROW, HEMATIZED FRACTURE ZONES 186.50-209.00: Banded 186.50-235.60: Medium Grained 204.40-210.20: Fractured FRACTURED WITH MINOR BRECCIA ZONES. ONLY WEAKLY HEMATITE ALTERED 209.00-235.60: Bedded 215.00-215.60: Fractured Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 235.60 236.30 IGRD, Granodiorite PINK TO RED GRANODIORITE BAND. MODERATELY HEMATIZED WITH BAND PARALLEL CONTACTS. 235.60-236.30: Hematite, Pervasive, Moderate Structure: 235.60-236.30: Foliation 235.60-236.30: Foliated 236.30 240.60 MQZT, Mafic metasediment QUETICO METASEDIMENTS. WEAK FRACTURE CONTROLLED HEMATITE AND CHLORITE ALTERATION. Page 12 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology 236.30-240.60: Carbonate, Fracture Filling, Weak 236.30-240.60: Chlorite, Fracture Filling, Weak 236.30-240.60: Hematite, Fracture Filling, Weak Mineralization: 236.30-240.60: Pyrite, Fracture Filling, 1% Structure: 236.30-240.60: Foliation 236.30-240.60: Medium Grained 236.30-240.60: Bedded Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 240.60 241.70 IMD, Mafic dykes ARCHEAN MAFIC DYKE. DARK GREEN/BLACK COLOUR. BIOTITE AND CHLORITE MAKE UP BULK OF COMPOSITION (LAMPROPHYRE?). STRONGLY FOLIATED TO SCHISTOSE, POSSIBLY SHEARED. 240.60-241.70: Carbonate, Fracture Filling, Weak Structure: 240.60-241.70: Sheared SHEARING IS BAND PARALLEL 240.60-241.70: Porphyritic BIOTITE PORPHYRITIC 240.60-241.70: Schistose 241.70 278.30 MQZT, Mafic metasediment QUETICO METASEDIMENTS. BACK TO A STRONG GNEISSIC TEXTURE FROM 242.7m TO 278.3m. STRONG HEMATITE ALTERATION FOLLOWS THE TEXTURAL CHANGE. 241.70-242.70: Hematite, Fracture Filling, Weak 241.70-278.30: Carbonate, Fracture Filling, Weak 241.70-278.30: Chlorite, Fracture Filling, Weak 242.70-257.00: Hematite, Pervasive, Strong 250.80-260.00: Epidote, Fracture Filling, Weak 257.00-278.30: Hematite, Pervasive, Weak 257.00-278.30: Hematite, Fracture Filling, Moderate Mineralization: 241.70-278.30: Pyrite, Fracture Filling, 1% XXXXXXXXX Page 13 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Structure: 241.70-278.30: Foliation 241.70-242.70: Bedded MASSIVE TO BEDDED 242.70-278.30: Banded GNEISSIC TEXTURE 250.60-254.00: Brecciated BRECCIATED BROKEN CORE. OPEN SPACE FILLING CARBONATE AND FELDSPAR IN PLACES Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 278.30 279.00 ITN, Tonalite STRONGLY HEMATIZED TONALITE PEGMATITE VEIN. QUARTZ, FELDSPAR, MUSCOVITE AND MINOR BIOTITE. 278.30-279.00: Hematite, Pervasive, Strong 278.30-279.00: Massive 278.30-279.00: Pegmatitic 279.00 281.50 MQZT, Mafic metasediment 279.00-281.50: Hematite, Pervasive, Moderate STRONGEST IN LEUCOCRATIC BANDS Mineralization: 279.00-281.50: Pyrite, Fracture Filling, 1% Structure: 279.00-281.50: Banded 279.00-281.50: Medium Grained 279.00-281.50: Banded 281.50 287.00 ITN, Tonalite STRONGLY HEMATIZED TONALITE PEGMATITE VEIN. QUARTZ, FELDSPAR, MUSCOVITE AND MINOR BIOTITE. 281.50-287.00: Hematite, Pervasive, Strong 281.50-287.00: Massive 281.50-287.00: Pegmatitic Page 14 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 287.00 289.70 MQZT, Mafic metasediment QUETICO METASEDIMENTS. MINOR FOLDING AND BOUDINAGING OF LEUCOSOME OBSERVED. 287.00-289.70: Chlorite, Fracture Filling, Weak 287.00-289.70: Hematite, Pervasive, Moderate STRONGEST ALTERATION ALONG LEUCOCRATIC BANDS Structure: 287.00-289.70: Banded 287.00-289.70: Folded DISCONTINOUS LEUCOSOME SHOWS FOLDING AT DRILL CORE SCALE 287.00-289.70: Medium Grained 287.00-289.70: Banded 289.70 290.80 ITN, Tonalite STRONGLY HEMATIZED TONALITE PEGMATITE VEIN. QUARTZ AND FELDSPAR COMPOSITION. 289.70-290.80: Hematite, Pervasive, Strong 289.70-290.80: Fractured 289.70-290.80: Massive 289.70-290.80: Pegmatitic 290.80 291.50 MQZT, Mafic metasediment 290.80-291.50: Hematite, Pervasive, Moderate Mineralization: 290.80-291.50: Pyrite, Fracture Filling, 1% Structure: 290.80-291.50: Foliation 290.80-291.50: Medium Grained 290.80-291.50: Banded 290.80-291.50: Fractured 291.50 292.20 ITN, Tonalite Page 15 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology STRONGLY HEMATIZED TONALITE PEGMATITE VEIN. QUARTZ AND FELDSPAR COMPOSITION. MODERATELY FRACTURED. 291.50-292.20: Carbonate, Fracture Filling, Weak 291.50-292.20: Hematite, Pervasive, Strong 291.50-292.20: Fractured 291.50-292.20: Massive 291.50-292.20: Pegmatitic Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 292.20 293.50 MQZT, Mafic metasediment DEEP RED, STRONGLY FRACTURED SEDIMENTS. ALTERATION HAS OBSCURED BANDING/BEDDING. 292.20-293.50: Epidote, Spots, Moderate APPEARS TO OVERPRINT ALL OTHER ALTERATION 292.20-293.50: Chlorite, Fracture Filling, Moderate 292.20-293.50: Hematite, Pervasive, Strong Mineralization: 292.20-293.50: Pyrite, Fracture Filling, 1% 292.20-293.50: Fine Grained 292.20-293.50: Foliated 293.50 295.30 ITN, Tonalite STRONGLY HEMATIZED TONALITE PEGMATITE VEIN. QUARTZ, FELDSPAR AND MINOR MUSCOVITE. MICROPERTHITE TEXTURE NOTED IN SOME FELDSPARS, WITH DARK RED HEMATIZED LAMELLAE. 293.50-295.30: Chlorite, Fracture Filling, Weak 293.50-295.30: Hematite, Pervasive, Strong 293.50-295.30: Fractured 293.50-295.30: Massive 293.50-295.30: Pegmatitic 295.30 296.30 MQZT, Mafic metasediment 295.30-296.30: Chlorite, Fracture Filling, Weak 295.30-296.30: Hematite, Pervasive, Weak Page 16 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Mineralization: 295.30-296.30: Pyrite, Fracture Filling, 1% Structure: 295.30-296.30: Banded 295.30-296.30: Medium Grained 295.30-296.30: Banded Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 296.30 296.60 ITN, Tonalite STRONGLY HEMATIZED TONALITE PEGMATITE VEIN. QUARTZ AND FELDSPAR COMPOSITION. 296.30-296.60: Hematite, Pervasive, Strong 296.30-296.60: Massive 296.30-296.60: Pegmatitic 296.60 298.80 MQZT, Mafic metasediment QUETICO METASEDIMENTS. FROM 297.4m STRONG FRACTURING, THEN BRECCIATION OBSERVED. CHLORITIC MATRIX WITH HEMATIZED FRAGMENTS OF SEDIMENT AND TONALITE. APPEARS TO BE A BRITTLE FAULT. SHARP CONTACT WITH UNDERLYING GABBRO IS BROKEN CORE. 296.60-297.40: Chlorite, Fracture Filling, Moderate 296.60-298.40: Hematite, Fracture Filling, Moderate 297.40-298.80: Chlorite, Fracture Filling, Strong 298.40-298.80: Hematite, Pervasive, Strong CLASTS WITHIN BRECCIA ZONE ARE STRONGLY HEMATIZED Mineralization: 296.60-298.80: Pyrite, Fracture Filling, 1% 296.60-297.40: Banded 297.40-298.20: Brecciated 297.40-298.20: Fault Gouge 298.80 299.60 IGD, Gabbroic dykes PYROXENE PHYRIC MAFIC DYKE. GREY/BLACK COLOUR. FINE GRAINED GROUNDMASS APPEARS CARBONATIZED. CARBONATE FRACTURES BREAK UP DYKE. 2-3% FRACTURE CONTROLLED PYRITE MINERALIZATION. 298.80-299.60: Carbonate, Fracture Filling, Strong Page 17 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Mineralization: 298.80-299.60: Pyrite, Fracture Filling, 2-3% 298.80-299.60: Massive 298.80-299.60: Fine Grained 298.80-299.60: Pyroxene Phyric Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 299.60 326.30 MQZT, Mafic metasediment BRECCIA/FAULT ZONE CONTINUES TO 299.9m. STRONGLY FRACTURED AFTERWARDS TO 300.3m. NARROW, ISOLATED FRACTURE/BRECCIA ZONES CONTINUE TO 306m AND ARE ASSOCIATED WITH STRONG HEMATITE ALTERATION. GNEISSIC TEXTURE THROUGH TO 326.3m. NARROW FRACTURES THROUGHOUT INTERVAL ARE OBSERVED TO DISPLACE BANDS 299.60-300.30: Chlorite, Fracture Filling, Strong 299.60-320.00: Epidote, Fracture Filling, Weak 299.60-320.00: Carbonate, Fracture Filling, Weak WEAK TO MODERATE CARBONATE FRACTURES INCREASE DOWNHOLE. XXXXXXXXXXXXXXXX 299.60-320.00: Hematite, Fracture Filling, Weak XXXXXXXXXXXX Mineralization: 299.60-326.30: Pyrite, Fracture Filling, 1% Structure: 299.60-326.30: Banded 299.60-306.00: Fractured 299.60-326.30: Medium Grained 299.60-326.30: Banded 326.30 337.20 ILMP, Lamprophyre BLACK-GREEN COARSE GRAINED BIOTITE/CHLORITE/AMPHIBOLE BEARING UNIT. UPPER AND LOWER CONTACTS ARE A MOTTLED GREEN-RED COLOUR, COMPRISED OF CRYPTOCRYSTALLINE CHLORITE/AMPHIBOLE? AND K-FELDSPAR. FROM 329.6 TO 330.1m UNIT LOOKS MORE GABBROIC, COMPRISED OF SUBHEDRAL AMPHIBOLE, PINK FELDSPAR AND UP TO 10% PYRITE. POSSIBLY A DYKE INTRUDING THIS UNIT? FROM 333.5-334.2m UNIT IS PEGMATITIC, WITH EUHEDRAL BLACK AMPHIBOLE AND K-FELDSPAR. 326.30-337.20: Carbonate, Fracture Filling, Weak 329.60-330.10: Epidote, Mottled, Moderate 329.60-330.10: Hematite, Mottled, Moderate 336.50-337.20: Chlorite, Mottled, Strong Mineralization: 329.60-330.10: Pyrite, Disseminated, 5% Page 18 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To 326.30-335.50: Coarse Grained 335.50-336.20: Pegmatitic 336.20-337.20: Coarse Grained Lithology 337.20 339.90 MQZT, Mafic metasediment GNEISSIC QUETICO METASEDIMENTS. FRACTURE FILLING HEMATITE AND CHLORITE ALTERATION THROUGHOUT. ABUNDANT HAIRLINE FRACTURES OF CARBONATE/HEMATITE. 337.20-339.90: Carbonate, Fracture Filling, Moderate 337.20-339.90: Chlorite, Fracture Filling, Moderate 337.20-339.90: Hematite, Fracture Filling, Moderate Mineralization: 337.20-339.90: Pyrite, Fracture Filling, 1% Structure: 337.20-339.90: Banded 337.20-339.90: Banded 337.20-339.90: Medium Grained 339.90 344.10 IMD, Mafic dykes GREEN, CHLORITIC, ARCHEAN MAFIC DYKE. POSSIBLY PART OF A SHEAR ZONE? STRONGLY FOLIATED. 339.90-344.10: Chlorite, Pervasive, Strong Mineralization: 339.90-344.10: Pyrite, Fracture Filling, 1% Structure: 339.90-344.10: Contact 339.90-344.10: Foliated 339.90-344.10: Fine Grained Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 344.10 355.50 MQZT, Mafic metasediment GNEISSIC QUETICO METASEDIMENTS. FRACTURE FILLING HEMATITE AND CHLORITE ALTERATION THROUGHOUT. FROM 352.8 TO LOWER CONTACT WITH GABBRO BRECCIA, STONGER PERVASSIVE HEMATITE ALTERATION GIVES CORE A DEEP RED-MAROON COLOUR. N500738 351.50 352.50 1.00 87.000 52.000 25.000 0.005 0.002 0.001 0.500 N500739 352.50 353.50 1.00 91.000 26.000 31.000 0.005 0.003 0.001 0.500 N500740 353.50 354.50 1.00 85.000 54.000 23.000 0.005 0.001 0.008 0.500 N500741 354.50 355.50 1.00 95.000 56.000 26.000 0.005 0.002 0.001 0.500 Page 19 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology 344.10-352.80: Hematite, Fracture Filling, Moderate 344.10-355.50: Carbonate, Fracture Filling, Moderate 344.10-355.50: Chlorite, Fracture Filling, Moderate 352.80-355.50: Hematite, Pervasive, Strong Mineralization: 344.10-355.50: Pyrite, Fracture Filling, 1% Structure: 344.10-355.50: Banded 344.10-355.50: Banded 344.10-355.50: Medium Grained Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 355.50 400.90 IGBX, Gabbro Breccia Page 20 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500742 355.50 356.50 1.00 49.000 67.000 23.000 0.010 0.007 0.001 0.500 N500742 355.50 356.50 1.00 49.000 67.000 23.000 0.010 0.007 0.001 0.500 N500743 356.50 357.50 1.00 47.000 74.000 23.000 0.013 0.010 0.001 0.500 N500743 356.50 357.50 1.00 47.000 74.000 23.000 0.013 0.010 0.001 0.500 N500744 357.50 358.50 1.00 7.000 56.000 5.000 0.005 0.003 0.012 0.500 N500745 358.50 359.20 0.70 5.000 11.000 3.000 0.005 0.002 0.001 0.500 N500746 359.20 359.50 0.30 18.000 11.000 13.000 0.009 0.007 0.001 0.500 N500747 359.50 360.40 0.90 11.000 15.000 6.000 0.007 0.004 0.001 0.500 N500748 360.40 361.50 1.10 28.000 54.000 17.000 0.011 0.007 0.001 0.500 N500749 361.50 362.50 1.00 15.000 25.000 11.000 0.005 0.003 0.001 0.500 N500751 362.50 363.50 1.00 14.000 21.000 9.000 0.005 0.002 0.001 0.500 N500752 363.50 364.70 1.20 2.000 6.000 2.000 0.005 0.001 0.001 0.500 N500753 364.70 365.50 0.80 29.000 67.000 17.000 0.005 0.003 0.001 0.500 N500754 365.50 366.50 1.00 48.000 50.000 23.000 0.007 0.004 0.001 0.500 N500755 366.50 367.50 1.00 53.000 43.000 22.000 0.008 0.007 0.001 0.500 N500756 367.50 368.50 1.00 33.000 45.000 17.000 0.005 0.004 0.001 0.500 N500757 368.50 369.50 1.00 31.000 71.000 19.000 0.005 0.003 0.001 0.500 N500758 369.50 371.00 1.50 35.000 36.000 18.000 0.005 0.003 0.001 0.500 N500759 371.00 372.50 1.50 35.000 52.000 21.000 0.006 0.004 0.001 0.500 N500761 372.50 374.00 1.50 43.000 83.000 22.000 0.007 0.005 0.001 0.500 N500762 374.00 375.50 1.50 22.000 47.000 14.000 0.009 0.006 0.001 0.500 N500763 375.50 377.00 1.50 29.000 91.000 17.000 0.012 0.008 0.001 0.500 N500764 377.00 378.50 1.50 35.000 70.000 20.000 0.007 0.005 0.001 0.500 N500765 378.50 380.00 1.50 35.000 107.000 20.000 0.007 0.006 0.001 0.500 N500766 380.00 381.50 1.50 32.000 70.000 19.000 0.006 0.005 0.001 0.500 N500767 381.50 383.00 1.50 37.000 42.000 19.000 0.010 0.007 0.001 0.500 N500768 383.00 384.50 1.50 38.000 43.000 18.000 0.008 0.006 0.001 0.500 N500769 384.50 386.00 1.50 36.000 91.000 18.000 0.005 0.003 0.001 0.500 N500771 386.00 387.50 1.50 40.000 146.000 20.000 0.005 0.005 0.001 0.500 N500772 387.50 389.00 1.50 42.000 62.000 17.000 0.006 0.003 0.001 0.500 N500773 389.00 390.50 1.50 41.000 102.000 20.000 0.007 0.005 0.001 0.500 N500774 390.50 392.00 1.50 31.000 51.000 17.000 0.007 0.006 0.001 0.500 N500775 392.00 393.50 1.50 30.000 49.000 16.000 0.006 0.005 0.001 0.500 N500776 393.50 395.00 1.50 31.000 89.000 16.000 0.020 0.013 0.001 0.500 N500777 395.00 396.50 1.50 27.000 6.000 18.000 0.006 0.004 0.001 0.500 N500778 396.50 398.00 1.50 43.000 102.000 19.000 0.021 0.016 0.001 0.500 N500779 398.00 399.00 1.00 56.000 109.000 21.000 0.028 0.025 0.001 0.500 N500780 398.00 399.00 1.00 58.000 114.000 21.000 0.031 0.025 0.001 0.500 N500781 399.00 400.00 1.00 153.000 128.000 28.000 0.113 0.101 0.004 0.500 N500782 400.00 400.90 0.90 50.000 122.000 26.000 0.036 0.034 0.001 0.500 N500744 357.50 358.50 1.00 7.000 56.000 5.000 0.005 0.003 0.012 0.500 N500745 358.50 359.20 0.70 5.000 11.000 3.000 0.005 0.002 0.001 0.500 N500746 359.20 359.50 0.30 18.000 11.000 13.000 0.009 0.007 0.001 0.500 N500747 359.50 360.40 0.90 11.000 15.000 6.000 0.007 0.004 0.001 0.500 N500748 360.40 361.50 1.10 28.000 54.000 17.000 0.011 0.007 0.001 0.500 N500749 361.50 362.50 1.00 15.000 25.000 11.000 0.005 0.003 0.001 0.500 Page 21 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500751 362.50 363.50 1.00 14.000 21.000 9.000 0.005 0.002 0.001 0.500 N500752 363.50 364.70 1.20 2.000 6.000 2.000 0.005 0.001 0.001 0.500 N500753 364.70 365.50 0.80 29.000 67.000 17.000 0.005 0.003 0.001 0.500 N500754 365.50 366.50 1.00 48.000 50.000 23.000 0.007 0.004 0.001 0.500 N500755 366.50 367.50 1.00 53.000 43.000 22.000 0.008 0.007 0.001 0.500 N500756 367.50 368.50 1.00 33.000 45.000 17.000 0.005 0.004 0.001 0.500 N500757 368.50 369.50 1.00 31.000 71.000 19.000 0.005 0.003 0.001 0.500 N500758 369.50 371.00 1.50 35.000 36.000 18.000 0.005 0.003 0.001 0.500 N500759 371.00 372.50 1.50 35.000 52.000 21.000 0.006 0.004 0.001 0.500 N500761 372.50 374.00 1.50 43.000 83.000 22.000 0.007 0.005 0.001 0.500 N500762 374.00 375.50 1.50 22.000 47.000 14.000 0.009 0.006 0.001 0.500 N500763 375.50 377.00 1.50 29.000 91.000 17.000 0.012 0.008 0.001 0.500 N500764 377.00 378.50 1.50 35.000 70.000 20.000 0.007 0.005 0.001 0.500 N500765 378.50 380.00 1.50 35.000 107.000 20.000 0.007 0.006 0.001 0.500 N500766 380.00 381.50 1.50 32.000 70.000 19.000 0.006 0.005 0.001 0.500 N500767 381.50 383.00 1.50 37.000 42.000 19.000 0.010 0.007 0.001 0.500 N500768 383.00 384.50 1.50 38.000 43.000 18.000 0.008 0.006 0.001 0.500 N500769 384.50 386.00 1.50 36.000 91.000 18.000 0.005 0.003 0.001 0.500 N500771 386.00 387.50 1.50 40.000 146.000 20.000 0.005 0.005 0.001 0.500 N500772 387.50 389.00 1.50 42.000 62.000 17.000 0.006 0.003 0.001 0.500 N500773 389.00 390.50 1.50 41.000 102.000 20.000 0.007 0.005 0.001 0.500 N500774 390.50 392.00 1.50 31.000 51.000 17.000 0.007 0.006 0.001 0.500 N500775 392.00 393.50 1.50 30.000 49.000 16.000 0.006 0.005 0.001 0.500 N500776 393.50 395.00 1.50 31.000 89.000 16.000 0.020 0.013 0.001 0.500 N500777 395.00 396.50 1.50 27.000 6.000 18.000 0.006 0.004 0.001 0.500 N500778 396.50 398.00 1.50 43.000 102.000 19.000 0.021 0.016 0.001 0.500 N500779 398.00 399.00 1.00 56.000 109.000 21.000 0.028 0.025 0.001 0.500 N500780 398.00 399.00 1.00 58.000 114.000 21.000 0.031 0.025 0.001 0.500 N500781 399.00 400.00 1.00 153.000 128.000 28.000 0.113 0.101 0.004 0.500 N500782 400.00 400.90 0.90 50.000 122.000 26.000 0.036 0.034 0.001 0.500 Page 22 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology MINOR INTERVALS: 355.50-357.50 : IGBX Gabbro Breccia BROWN/MAROON COLOURED GABBROIC MATRIX WITH ABUNDANT SUBANGULAR XENOLITHS (30-40%). XENOLITHS ARE DOMINANTLY QUARTZ WITH BLACK CHLORITIC CORONAS AND MINOR CLASTS OF BLACK QUETICO SEDIMENT WHICH ARE MORE SUBROUNDED IN SHAPE AND OBSERVED TO BE PARTIALLY DIGESTED INTO THE GABBRO. PODS/CLASTS OF EPIDOTE RICH MATERIAL COMMON. 2-5% CARBONATE CLASTS ARE FINE GRAINED, SOMETIMES ASSOCIATED WITH QUARTZ XENOLITHS. 1-3% DISSEMINATED PYRITE. 357.50-359.20 : IGRD IGRD DARK RED, HEMATIZED GRANODIORITE. LIKELY A LARGE WALL ROCK XENOLITH. DIFFUSE CONTACTS WITH GABBRO WHICH APPEARS TO BE DIGESTING GRANODIORITE. NARROW DIFFUSE ZONES OF QUARTZ XENOLITH BEARING GABBRO WITHIN THIS INTERVAL. 359.20-359.50 : IGBX Gabbro Breccia BRIGHT RED QUARTZ XENOLITH BEARING GABBRO BRECCIA. DIFFUSE UPPER AND LOWER CONTACTS WITH GRANODIORITE. 359.50-360.40 : IGRD IGRD BRIGHT RED GRANODIORITE AS ABOVE, AGAIN WITH NARROW ZONES OF GABBRO BRECCIA X-CUTTING INTERVAL. 360.40-363.50 : IGBX Gabbro Breccia BRIGHT RED GABBRO BRECCIA. XENOLITHS OF QUARTZ AND GRANODIORITE COMPRISE 30% OF INTERVAL. 363.50-364.70 : IGRD IGRD BRIGHT RED/PINK GRANODIORITE XENOLITH. 364.70-400.90 : IGBX Gabbro Breccia BRIGHT RED TO GREY COLOURED GABBRO BRECCIA. AS ABOVE, UNIT IS CHARACTERIZED BY A RED AND BLACK, FINE GRAINED, HEMATIZED GABBROIC GROUNDMASS WITH ~20% SUBANGULAR QUARTZ XENOLITHS. QUARTZ XENOLITHS RANGE FROM 1-20cm LONG AND HAVE A NARROW, CHLORITIC HALO SURROUNDING THEM. PATCHY EPIDOTE ALTERATION FOUND IN AND ADJACENT TO SOME XENOLITHS. 1-4% DISSEMINATED PYRITE THROUGHOUT. PYRITE IS MOST ABUNDANT FROM 399.5m. LOWER CONTACT WITH UPPER SERIES GABBRO IS OCCURS OVER ~1m WHERE GROUNDMASS GRADUALLY COARSENS, SHOWING EUHEDRAL FELDSPAR AND AMPHIBOLE, AND QUARTZ XENOLITHS CEASE. Minor 355.50-357.50: Epidote, Patchy, Weak 355.50-357.50: Hematite, Pervasive, Strong 357.50-359.20: Hematite, Pervasive, Strong 359.20-359.50: Hematite, Pervasive, Strong 359.50-360.40: Hematite, Pervasive, Strong 360.40-363.50: Hematite, Pervasive, Strong 363.50-364.70: Hematite, Pervasive, Strong 364.70-367.50: Hematite, Pervasive, Strong 367.50-370.30: Epidote, Patchy, Moderate SPOTS OF EPIDOTE MAY REPRESENT ALTERED XENOLITHS 367.90-388.00: Hematite, Pervasive, Strong 388.40-400.90: Hematite, Pervasive, Strong Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 23 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Minor Mineralization: Lithology 355.50-357.50: Pyrite, Disseminated, 1-3% 359.20-359.50: Pyrite, Fracture Filling, 2% 359.50-360.40: Pyrite, Disseminated, 2% MINERALIZATION CONFINED TO NARROW INTERVALS OF GABBRO BRECCIA CUTTING GRANODIO 360.40-363.50: Pyrite, Disseminated, 2% FINELY DISSEMINATED PYRITE ALONG WITH FRACTURE FILLING PYRITE 364.70-380.00: Pyrite, Disseminated, 4% FINELY DISSEMINATED THROUGH MATRIX AND LESSER MEDIUM GRAINED EUHEDRAL PYRITE 380.00-399.50: Pyrite, Disseminated, 2% FINELY DISSEMINATED BUT PATCHY 380.00-400.90: Pyrite, Disseminated, 4% COARSER DISSEMINATED PYRITE. STARTING TO CONCENTRATE ADJACENT AND WITHIN XENOL Minor 355.50-357.50: Xenolithic QUARTZ, CARBONATE, AND QUETICO XENOLITHS 355.50-357.50: Fine Grained Matrix 357.50-359.20: Massive 357.50-359.20: Medium Grained 359.20-359.50: Xenolithic 359.20-359.50: Fine Grained Matrix 359.50-360.40: Medium Grained 359.50-360.40: Massive 360.40-363.50: Fine Grained Matrix 360.40-363.50: Xenolithic QUARTZ AND GRANODIORITE XENOLITHS 363.50-364.70: Massive 363.50-364.70: Medium Grained 364.70-400.90: Xenolithic APPROXIMATELY 20% XENLOLITHS ARE DOMINANTLY SUBANGULAR QUARTZ. AS LOWER CONTACT IS APPROACHED, CHLORITE HALO SURROUNDING QUARTZ BECOMES WIDER. FRAGMENTS OF CHLORITE/AMPHIBOLE APPEAR NEAR LOWER CONTACT. 364.70-400.90: Fine Grained Matrix 393.50-397.60: Fractured VERY FRACTURED, BROKEN CORE. NOT GRAVEL Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 400.90 421.50 IGUS, Upper Series Gabbro Page 24 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct N500783 400.90 402.00 1.10 10.000 35.000 36.000 0.005 0.001 0.001 0.500 N500783 400.90 402.00 1.10 10.000 35.000 36.000 0.005 0.001 0.001 0.500 N500784 402.00 403.00 1.00 33.000 105.000 45.000 0.005 0.001 0.002 0.500 N500784 402.00 403.00 1.00 33.000 105.000 45.000 0.005 0.001 0.002 0.500 N500785 403.00 404.00 1.00 31.000 29.000 49.000 0.005 0.001 0.001 0.500 N500785 403.00 404.00 1.00 31.000 29.000 49.000 0.005 0.001 0.001 0.500 N500786 404.00 405.50 1.50 33.000 165.000 39.000 0.007 0.002 0.001 0.500 N500786 404.00 405.50 1.50 33.000 165.000 39.000 0.007 0.002 0.001 0.500 N500787 405.50 407.00 1.50 27.000 153.000 38.000 0.005 0.001 0.001 0.500 N500787 405.50 407.00 1.50 27.000 153.000 38.000 0.005 0.001 0.001 0.500 N500788 407.00 408.50 1.50 12.000 81.000 36.000 0.005 0.001 0.001 0.500 N500788 407.00 408.50 1.50 12.000 81.000 36.000 0.005 0.001 0.001 0.500 N500789 408.50 410.00 1.50 13.000 105.000 38.000 0.005 0.001 0.001 0.500 N500789 408.50 410.00 1.50 13.000 105.000 38.000 0.005 0.001 0.001 0.500 N500791 410.00 411.50 1.50 49.000 267.000 45.000 0.017 0.003 0.004 0.500 N500791 410.00 411.50 1.50 49.000 267.000 45.000 0.017 0.003 0.004 0.500 N500792 411.50 413.00 1.50 65.000 256.000 47.000 0.027 0.006 0.006 0.500 N500792 411.50 413.00 1.50 65.000 256.000 47.000 0.027 0.006 0.006 0.500 N500793 413.00 414.50 1.50 52.000 314.000 43.000 0.016 0.003 0.004 0.500 N500793 413.00 414.50 1.50 52.000 314.000 43.000 0.016 0.003 0.004 0.500 N500794 414.50 416.00 1.50 55.000 263.000 44.000 0.020 0.007 0.003 0.500 N500794 414.50 416.00 1.50 55.000 263.000 44.000 0.020 0.007 0.003 0.500 N500795 416.00 417.50 1.50 63.000 246.000 48.000 0.022 0.010 0.003 0.500 N500795 416.00 417.50 1.50 63.000 246.000 48.000 0.022 0.010 0.003 0.500 N500796 417.50 418.50 1.00 72.000 160.000 44.000 0.029 0.015 0.006 0.500 N500796 417.50 418.50 1.00 72.000 160.000 44.000 0.029 0.015 0.006 0.500 N500797 418.50 419.50 1.00 67.000 209.000 42.000 0.029 0.018 0.004 0.500 N500797 418.50 419.50 1.00 67.000 209.000 42.000 0.029 0.018 0.004 0.500 N500798 419.50 420.50 1.00 80.000 248.000 50.000 0.025 0.010 0.006 0.500 N500798 419.50 420.50 1.00 80.000 248.000 50.000 0.025 0.010 0.006 0.500 N500799 420.50 421.50 1.00 93.000 257.000 58.000 0.022 0.014 0.003 0.500 N500799 420.50 421.50 1.00 93.000 257.000 58.000 0.022 0.014 0.003 0.500 MINOR INTERVALS: 400.90-421.50 : ILGB Leucogabbro PLAGIOCLASE CUMULATE LEUCOGABBRO/MONZOGABBRO. RED AND GREEN SPOTTED APPEARANCE TO 404m DUE TO PODS OF CHLORITE/AMPHIBOLE WITHIN HEMATIZED GROUNDMASS. FELDSPAR ARE EUHDERAL, LATH SHAPED THROUGHOUT INTERVAL WITH EUHEDRAL AMPHIBOLE/PYROXENE BECOMING MORE PROMINENT DOWN HOLE. INTERCUMULUS GROUNDMASS IS STRONGLY HEMATIZED, FINE GRAINED AND ANHEDRAL. 1-2 % DISSEMINATED PYRITE THROUGHOUT. UNIT BECOMES SLIGHTLY MORE MAFIC DOWNHOLE BEFORE GRADATIONAL LOWER CONTACT WITH FINER GRAINED LOWER SERIES GABBRO. Page 25 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Minor Lithology 400.90-421.50: Sericite, Pervasive, Moderate ALL FELDSPAR APPEARS SERICITIZED 400.90-421.50: Epidote, Patchy, Moderate 400.90-421.50: Hematite, Mottled, Strong HEMATITE ALTERATION FOCUSED WITHIN PODS/MASSES OF ANHEDRAL GROUNDMASS SURROUNDING PLAGIOCLASE LATHS Minor Mineralization: 400.90-402.50: Pyrite, Disseminated, 4% DISSEMINATED AND FRACTURE CONTROLLED PYRITE 402.50-421.50: Pyrite, Disseminated, 1% Minor 400.90-421.50: Medium Grained - Coarse Grained EUHEDRAL PLAGIOCLASE LATHS AND AMPHIBOLE/PYROXENE 400.90-421.50: Mesocumulate PLAGIOCLASE CUMULATE 421.50 446.10 IGLS, Lower Series Gabbro Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 26 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct J591300 421.50 422.50 1.00 194.000 124.000 63.000 0.019 0.006 0.001 0.500 J591300 421.50 422.50 1.00 194.000 124.000 63.000 0.019 0.006 0.001 0.500 J591301 422.50 423.50 1.00 225.000 161.000 67.000 0.029 0.018 0.005 0.500 J591301 422.50 423.50 1.00 225.000 161.000 67.000 0.029 0.018 0.005 0.500 J591302 423.50 424.50 1.00 235.000 142.000 68.000 0.017 0.009 0.002 0.500 J591302 423.50 424.50 1.00 235.000 142.000 68.000 0.017 0.009 0.002 0.500 J591303 424.50 425.50 1.00 244.000 148.000 72.000 0.018 0.007 0.002 0.500 J591303 424.50 425.50 1.00 244.000 148.000 72.000 0.018 0.007 0.002 0.500 J591304 425.50 426.50 1.00 259.000 140.000 73.000 0.025 0.010 0.002 0.500 J591304 425.50 426.50 1.00 259.000 140.000 73.000 0.025 0.010 0.002 0.500 J591305 426.50 427.50 1.00 273.000 149.000 72.000 0.024 0.013 0.002 0.500 J591305 426.50 427.50 1.00 273.000 149.000 72.000 0.024 0.013 0.002 0.500 J591306 427.50 428.50 1.00 273.000 142.000 69.000 0.014 0.004 0.001 0.500 J591306 427.50 428.50 1.00 273.000 142.000 69.000 0.014 0.004 0.001 0.500 J591307 428.50 429.50 1.00 274.000 121.000 70.000 0.021 0.008 0.001 0.500 J591307 428.50 429.50 1.00 274.000 121.000 70.000 0.021 0.008 0.001 0.500 J591308 429.50 430.50 1.00 286.000 163.000 70.000 0.050 0.029 0.005 0.500 J591308 429.50 430.50 1.00 286.000 163.000 70.000 0.050 0.029 0.005 0.500 J591310 430.50 431.50 1.00 289.000 216.000 71.000 0.032 0.020 0.004 0.500 J591310 430.50 431.50 1.00 289.000 216.000 71.000 0.032 0.020 0.004 0.500 J591311 431.50 432.50 1.00 250.000 230.000 69.000 0.024 0.012 0.001 0.500 J591311 431.50 432.50 1.00 250.000 230.000 69.000 0.024 0.012 0.001 0.500 J591312 432.50 433.20 0.70 219.000 181.000 66.000 0.036 0.022 0.002 0.500 J591312 432.50 433.20 0.70 219.000 181.000 66.000 0.036 0.022 0.002 0.500 J591313 433.20 434.00 0.80 371.000 223.000 73.000 0.084 0.057 0.006 0.500 J591313 433.20 434.00 0.80 371.000 223.000 73.000 0.084 0.057 0.006 0.500 J591314 434.00 434.70 0.70 331.000 695.000 70.000 0.083 0.056 0.011 0.500 J591314 434.00 434.70 0.70 331.000 695.000 70.000 0.083 0.056 0.011 0.500 J591315 434.70 435.50 0.80 250.000 166.000 69.000 0.044 0.021 0.001 0.500 J591315 434.70 435.50 0.80 250.000 166.000 69.000 0.044 0.021 0.001 0.500 J591316 435.50 436.50 1.00 410.000 1,310.000 90.000 0.178 0.127 0.014 0.500 J591316 435.50 436.50 1.00 410.000 1,310.000 90.000 0.178 0.127 0.014 0.500 J591317 436.50 437.50 1.00 231.000 377.000 73.000 0.026 0.013 0.003 0.500 J591317 436.50 437.50 1.00 231.000 377.000 73.000 0.026 0.013 0.003 0.500 J591318 437.50 438.50 1.00 221.000 355.000 72.000 0.042 0.029 0.004 0.500 J591319 437.50 438.50 1.00 212.000 336.000 67.000 0.045 0.033 0.004 0.500 J591318 437.50 438.50 1.00 221.000 355.000 72.000 0.042 0.029 0.004 0.500 J591319 437.50 438.50 1.00 212.000 336.000 67.000 0.045 0.033 0.004 0.500 J591320 438.50 439.50 1.00 187.000 222.000 65.000 0.030 0.020 0.002 0.500 J591320 438.50 439.50 1.00 187.000 222.000 65.000 0.030 0.020 0.002 0.500 J591321 439.50 440.50 1.00 186.000 167.000 63.000 0.027 0.014 0.002 0.500 J591321 439.50 440.50 1.00 186.000 167.000 63.000 0.027 0.014 0.002 0.500 J591322 440.50 441.50 1.00 199.000 212.000 62.000 0.049 0.029 0.017 0.500 J591322 440.50 441.50 1.00 199.000 212.000 62.000 0.049 0.029 0.017 0.500 J591323 441.50 442.50 1.00 219.000 380.000 64.000 0.063 0.025 0.009 0.500 J591323 441.50 442.50 1.00 219.000 380.000 64.000 0.063 0.025 0.009 0.500 Page 27 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct J591324 442.50 443.50 1.00 175.000 375.000 64.000 0.040 0.022 0.006 0.500 J591324 442.50 443.50 1.00 175.000 375.000 64.000 0.040 0.022 0.006 0.500 J591325 443.50 444.50 1.00 142.000 263.000 64.000 0.024 0.026 0.004 0.500 J591325 443.50 444.50 1.00 142.000 263.000 64.000 0.024 0.026 0.004 0.500 J591326 444.50 445.20 0.70 242.000 431.000 62.000 0.055 0.049 0.004 0.500 J591326 444.50 445.20 0.70 242.000 431.000 62.000 0.055 0.049 0.004 0.500 J591327 445.20 445.50 0.30 372.000 191.000 73.000 0.098 0.057 0.012 0.500 J591327 445.20 445.50 0.30 372.000 191.000 73.000 0.098 0.057 0.012 0.500 J591328 445.50 446.10 0.60 216.000 263.000 57.000 0.058 0.030 0.001 0.500 J591328 445.50 446.10 0.60 216.000 263.000 57.000 0.058 0.030 0.001 0.500 MINOR INTERVALS: 421.50-446.10 : IGB Gabbro RAPID BUT DIFFUSE CONTACT WITH OVERLYING COARSE GRAINED UPPER SERIES GABBRO MARKED BY DECREASE IN GRAINSIZE AND FELDSPAR CONTENT. FINE TO MEDIUM GRAINED GREY GABBRO WITH WEAK HEMATITE ALTERATION FROM 431.5m STAINING FELDSPAR. 2-3% SULFIDE THROUGHOUT ENTIRE INTERVAL BUT MOSTLY PY-PO. 2% COARSE BLEBBY CPY-PO FROM 434-434.6m. SHARP INTERNAL CONTACT AT 433.2m SEPARATES MEDIUM GRAINED HEMATIZED GABBRO FROM UNDERLYING FINE GRAINED MELAGABBRO UNIT WHICH APPEARS TO BE MODERATELY URALITIZED. THIS UNIT THEN COARSENS, WITH HEMATIZED FELDSPAR BECOMING MORE ABUNDANT, DOWNHOLE. UNALTERED "DYKE" OF SIMILAR GABBRO CUTS HEMATIZED GABBRO AT 445.2-445.6m. NO CHILLED MARGINS ON DYKE. AT CONTACT THE GABBRO AND FOOTWALL GRANODIORITE ARE STRONGLY HEMATIZED. 2% COARSER BLEBBY/BLOCKY PYRRHOTITE MINERALIZATION AT CONTACT. Minor 431.80-433.20: Hematite, Pervasive, Moderate RED STAINING OF FELDSPAR 433.20-436.00: Hornblende, Pervasive, Moderate URALITIZATION OF PYROXENE THROUGH THIS INTERVAL 434.70-446.10: Hematite, Pervasive, Moderate RED STAINING OF FELDSPAR Minor Mineralization: 421.50-434.00: Pyrrhotite/Pyrite, Disseminated, 2-3% FINELY DISSEMINATED SULFIDE THROUGHOUT INTERVAL. AGGREGATES OF FINE SULFIDE FOR 434.00-434.60: Pyrrhotite/Chalcopyrite, Blebby, 2% COARSE GRAINED BLEBS OF FRACTIONATED SULFIDE THROUGH THIS INTERVAL 434.60-446.10: Pyrrhotite/Pyrite, Disseminated, 2-3% FINELY DISSEMINATED SULFIDE WITH COARE BLOCKS/BLEBS AT BASAL CONTACT Page 28 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology Minor Structure: 433.20-433.20: Contact INTERNAL CONTACT 445.20-445.20: Contact INTERNAL CONTACT OR DYKE? 446.10-446.10: Contact IRREGULAR, BASAL CONTACT Minor 421.50-431.50: Fine Grained 431.50-433.20: Medium Grained - Coarse Grained 433.20-433.20: Oikocrysts FELDSPAR OIKOCRYSTS THROUGHOUT 433.20-433.40: Xenolithic FRAGMENTS OF OVERLYING MEDIUM GRAINED GABBRO 433.20-446.10: Fine Grained - Medium Grained GRADUALLY COARSENS AWAY FROM INTERNAL CONTACT. NO CHILLED MARGIN AT CONTACT 438.20-438.20: Coarse Grained COARSE GRAINED HEMATITIZED VEINS Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 446.10 460.20 IGRD, Granodiorite DARK RED TO PINK GRANODIORITE. CONTACT ALTERATION EVIDENT BY DEEP RED COLOUR OF GRANODIORITE WHICH GRADUALLY WEAKENS AWAY FROM THE INTRUSION. FRACTURED BROKEN CORE FROM 447.5-460.2m. STRONG FOLIATION EVIDENT AWAY FROM CONTACT ALTERATION. CHLORITE FOUND ALONG FRACTURE SURFACES. FELDSPAR PORPHYRITIC. SHARP CONTACT WITH UNDERLYING METASEDIMENTS. J591330 446.10 447.00 0.90 3.000 4.000 2.000 0.005 0.001 0.001 0.500 J591331 447.00 448.00 1.00 1.000 2.000 1.000 0.005 0.001 0.001 0.500 J591332 448.00 449.00 1.00 3.000 3.000 1.000 0.005 0.001 0.001 0.500 J591333 449.00 450.00 1.00 2.000 2.000 1.000 0.005 0.001 0.001 0.500 446.10-447.50: Hematite, Pervasive, Strong 446.10-460.20: Chlorite, Fracture Filling, Moderate 447.50-460.20: Hematite, Pervasive, Moderate MODERATE TO WEAK DOWNHOLE Structure: 446.10-460.20: Foliation 446.10-460.20: Coarse Grained 447.50-460.20: Broken Core 450.80-460.20: Porphyritic FELDSPAR PHYRIC 451.30-451.40: Brecciated 460.20 469.30 MQZT, Mafic metasediment Page 29 of 31 Feb 13, 2015

Hole Number: SL-14-007 From To Lithology QUETICO METASEDIMENTS. MODERATE HEMATITE ALTERATION THROUGHOUT, PREFERENTIALLY ALTERING ALONG FRACUTURES AND LEUCOCRATIC BANDS. 460.20-469.30: Hematite, Fracture Filling, Moderate ALTERATION FOLLOWS FRACTURES OR LEUCOCRATIC BANDS. ALTERATION IS WEAKLY PERVASSIVE AS WELL Mineralization: 460.20-469.30: Pyrite, Fracture Filling, 1% Structure: 460.20-469.30: Banded 460.20-469.30: Fractured WEAKLY FRACTURED 460.20-469.30: Medium Grained 460.20-469.30: Banded Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 469.30 472.00 IGRD, Granodiorite AS ABOVE, FOLIATED, FELDSPAR PHYRIC GRANODIORITE. MODERATELY HEMATIZED. 469.30-472.00: Hematite, Pervasive, Moderate Structure: 469.30-472.00: Foliation 469.30-472.00: Porphyritic FELDSPAR PHYRIC 469.30-472.00: Coarse Grained 469.30-472.00: Foliated 472.00 497.00 MQZT, Mafic metasediment QUETICO METASEDIMENTS. STRONGLY BANDED QUETICO SEDIMENTS. MINOR, VERY WEAK HEMATITE ALTERATION IS ABSENT BY 480m. 472.00-480.00: Hematite, Pervasive, Weak Structure: 472.00-497.00: Banded 472.00-497.00: Medium Grained 472.00-497.00: Banded Page 30 of 31 Feb 13, 2015

Hole Number: SL-14-007 Survey Data Depth Azimuth Decimal Dip Decimal Test Type Flag 0.00 295.00-78.00 REFLEX O 32.00 290.80-77.40 REFLEX O 62.00 286.70-76.50 REFLEX O 92.00 288.40-75.80 REFLEX O 152.00 290.00-74.30 REFLEX O 182.00 280.40-73.50 REFLEX O 212.00 276.90-72.40 REFLEX O 242.00 279.30-71.10 REFLEX O 272.00 284.00-69.90 REFLEX O 302.00 273.00-69.20 REFLEX O 362.00 282.70-67.10 REFLEX O 422.00 280.00-65.90 REFLEX O 482.00 280.00-65.90 REFLEX O Comments Page 31 of 31 Feb 13, 2015

Hole Number SL-14-008 Project Name: Project Code: Location: Start Date: Completed Date: Contractor: Core Storage: Units: Comments: Detailed Lithology From To Project SUNDAY LAKE 23 Dec 11, 2014 Jan 19, 2015 Orbit Garant TMC Core Shack METRIC Coordinates Primary Coordinates Grid: UTM83-16 North: 5,395,189.00 East: 334,714.00 Elev: 484.00 Destination Coordinates Grid: LL83 North: East: Elev: 48.69-89.25 484.00 Collar Dip: Length: Hole Size: Hole Type: Casing: Collar Survey: N Multishot Survey: N -85.00 Collar Az: 290.00 714.00 NQ DD Left in Hole DRILL HOLE TO TEST CONTINUITY OF MINERALIZATION AND GEOLOGY BETWEEN SL-13-006 & SL-14-006. HOLE WILL CROSS OVER NW TRENDING GRAVITY/MAGNETIC LINEAMENT. Lithology 0.00 6.00 CAS, CASING AND OVERBURDEN 6.00 66.60 MQZT, Mafic metasediment QUEITCO METASEDIMENTS. INTERVAL IS MODERATELY TO STRONGLY FRACTURED, WITH NARROW BRECCIA ZONES AS INDICATED IN TEXTURE LOG. HEMATITE ALTERATION IS PRESENT THROUGHOUT INTERVAL, CONCENTRATED ALONG FRACTURED/BRECCIATED ZONES. 6.00-66.60: Sericite, Fracture Filling, Weak BLEACHED HALOS AROUND NARROW FRACTURES 6.00-66.60: Epidote, Fracture Filling, Weak 9.00-10.50: Hematite, Pervasive, Strong 18.00-19.50: Chlorite, Veins, Moderate QUARTZ PEGMATITE VEIN WITH CHLORITE ALONG MARGINS 20.50-38.20: Hematite, Fracture Filling, Strong HEMATITE STAINING PERMEATES FROM FRACTURES AND BRECCIA ZONES. 38.20-40.00: Hematite, Pervasive, Strong BRECCIA ZONE 40.00-51.60: Hematite, Fracture Filling, Weak 51.60-52.30: Hematite, Pervasive, Strong 52.30-58.10: Hematite, Fracture Filling, Moderate 58.10-58.60: Hematite, Fracture Filling, Strong 58.60-66.60: Hematite, Fracture Filling, Strong 58.60-66.60: Hematite, Pervasive, Weak Sample # Collar Plugged: N Pulse EM Survey: N From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 1 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology Mineralization: 6.00-66.60: Pyrite, Fracture Filling, 1-2% Structure: 6.00-66.60: Banded 6.00-66.60: Medium Grained 6.00-66.60: Banded 8.50-10.00: Broken Core 32.80-34.50: Broken Core 38.20-40.00: Brecciated STRONGLY HEMATIZED BRECCIA ZONE. BROKEN CORE 38.20-41.70: Broken Core 51.60-52.30: Brecciated 56.00-56.90: Broken Core 58.10-58.40: Brecciated STRONGLY HEMATIZED BRECCIA ZONE Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 66.60 67.40 IMD, Mafic dykes ARCHEAN MAFIC DYKE. CHLORITIC, STRONGLY FOLIATED WITH BANDS OF QUARTZ/FELDSPAR. BANDS SHOW DEXTRAL DISPLACEMENT ALONG NARROW FRACTURES. 66.60-67.40: Hematite, Pervasive, Moderate 66.60-67.40: Chlorite, Pervasive, Strong Structure: 66.60-67.40: Foliation 66.60-67.40: Fine Grained 66.60-67.40: Foliated 67.40 326.40 MQZT, Mafic metasediment QUETICO METASEDIMENTS. FROM 67.4-153.8m CORE IS DEEP RED/MAROON COLOUR DUE TO PERVASSIVE HEMATITE ALTERATION. STRONG ALTERATION IS FOCUSED ALONG FRACTURES AND WITHIN NARROW BRECCIA ZONES. FRACTURES SHOW SMALL AMOUNTS OF DEXTRAL DISPLACEMENT ON BEDS/BANDS. FROM 153.8-208.3m PERVASSIVE HEMATITE ALTERATION IS NEARLY ABSENT, BEING CONFINED TO FRACTURED/BRECCIATED INTERVALS AS INDICATED IN ALTERATION LOG. CORE FROM 153.8m-160.5m HAS ABUNDANT FRACTURES WITH BLEACHED HALOS (SERICITE?). FROM 208.3-293.2m FRACTURING, BRECCIATION AND HEMATITE ALTERATION BECOME STRONGER. CHLORITE ALTERATION IN FRACTURES ALSO MORE PROMINENT. FROM 293.2-326.4m FRACTURING, ALTERATION AND BRECCIATION IS LESS PROMINENT. FROM 310.5m GNEISSIC TEXTURE IS LOST, APPEARING MORE BEDDED. Page 2 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology 67.40-91.50: Hematite, Pervasive, Weak 67.40-92.20: Sericite, Fracture Filling, Weak BLEACHED HALOS AROUND NARROW FRACTURES. 67.40-153.80: Chlorite, Fracture Filling, Moderate 91.50-92.20: Hematite, Pervasive, Strong BRECCIA ZONE 92.20-153.80: Hematite, Fracture Filling, Strong 92.20-153.80: Hematite, Pervasive, Moderate 136.50-136.80: Carbonate, Fracture Filling, Moderate PART OF MATRIX IN BRECCIA ZONE 153.80-160.50: Hematite, Fracture Filling, Weak 153.80-208.30: Sericite, Fracture Filling, Weak 160.50-160.90: Chlorite, Fracture Filling, Moderate 160.50-160.90: Hematite, Fracture Filling, Strong 160.90-175.50: Hematite, Fracture Filling, Weak 175.90-185.20: Hematite, Fracture Filling, Weak 185.20-185.80: Hematite, Fracture Filling, Strong 185.80-189.40: Hematite, Fracture Filling, Weak 189.40-193.50: Hematite, Fracture Filling, Moderate 191.00-192.80: Sericite, Fracture Filling, Strong GREEN/GREY ALTERATION IN BRECCIA ZONE 193.50-207.80: Hematite, Fracture Filling, Weak 207.80-208.30: Hematite, Pervasive, Strong 208.30-245.20: Hematite, Pervasive, Moderate 208.30-293.20: Hematite, Fracture Filling, Strong 210.00-326.40: Chlorite, Fracture Filling, Moderate CHLORITE FOUND IN CORES OF HEMATITIC FRACTURES AND AS MATRIX WITHIN BRECCIA ZONES 240.00-326.40: Sericite, Fracture Filling, Weak NARROW FRACTURES WITH BLEACHED HALOS. SOMETIMES ASSOCIATED WITH CHLORITE 254.30-260.40: Epidote, Fracture Filling, Moderate 259.00-300.60: Hematite, Pervasive, Moderate 293.20-300.60: Hematite, Fracture Filling, Moderate 300.60-308.00: Hematite, Pervasive, Strong 300.60-308.00: Hematite, Fracture Filling, Strong 308.00-323.10: Hematite, Pervasive, Weak 308.00-323.10: Hematite, Fracture Filling, Moderate 323.10-326.40: Hematite, Pervasive, Moderate Mineralization: 67.40-326.40: Pyrite, Fracture Filling, 1-2% Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 3 of 20 Feb 13, 2015

Hole Number: SL-14-008 From Structure: To Lithology 67.40-67.40: Banded 300.00-300.00: Banded 67.40-310.50: Banded 67.40-326.40: Medium Grained 91.50-92.20: Brecciated 98.60-99.00: Broken Core 102.80-103.10: Brecciated 109.40-109.60: Broken Core 110.70-111.00: Broken Core 110.70-185.80: Fractured FRACTURED, BRECCIATED AND BROKEN CORE IN THIS INTERVAL. FRACTURES SHOW SMALL AMOUNTS OF DEXTRAL DISPLACEMENT 119.30-122.30: Broken Core 119.30-123.20: Brecciated 130.20-130.70: Brecciated BRECCIA CLASTS SHOW CORONA TEXTURES WITH UNALTERED CORES 136.50-136.80: Brecciated 147.00-153.80: Brecciated 189.40-192.80: Brecciated 213.00-213.50: Brecciated 213.00-293.20: Fractured ENTIRE INTERVAL RIDDLED WITH HEMATITIC FRACTURES ALONG WITH NARROWER BLEACHED FRACTURES 224.40-227.80: Brecciated 224.40-227.80: Broken Core 245.20-245.70: Brecciated 264.10-264.50: Broken Core 285.30-285.80: Brecciated 300.60-303.00: Brecciated STRONGLY FRACTURED TO BRECCIATED 310.50-326.40: Bedded 323.10-323.70: Broken Core 323.10-326.40: Fractured 326.40 328.00 IMD, Mafic dykes ARCHEAN MAFIC DYKE. GREEN, STRONGLY FOLIATED AND COMPRISED OF CHLORITE, AMPHIBOLE AND K-FELDSPAR. FROM 327.5 327.8m STRONG CHLORITE VEINS IN BRECCIA ZONE. 326.40-328.00: Chlorite, Pervasive, Moderate Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 4 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology Structure: 326.40-326.40: Contact CONTACT IS SLIGHTLY OBLIQUE TO GNEISSIC BANDING IN SEDIMENTS 326.40-328.00: Foliation 328.00-328.00: Contact CONTACT IS SLIGHTLY OBLIQUE TO GNEISSIC BANDING IN SEDIMENTS 326.40-328.00: Medium Grained 326.40-328.00: Schistose 327.50-327.80: Brecciated Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 328.00 347.90 MQZT, Mafic metasediment QUETICO METASEDIMENTS. GENERALLY MASSIVE TO BEDDED WITH BANDED PEGMATITE VEIN FROM 335.8-337m. WEAKER ALTERATION UNTIL 335.8m AFTER WHICH PERVASSIVE AND FRACTURE CONTROLLED HEMATITE ALTERATION IS STRONG. FRACTURES SHOW A CORE OF PYRITE, FOLLOWED BY CHLORITE WITH HEMATITE RADIATING AWAY FROM FRACTURE INTO COMPETENT ROCK. 328.00-335.80: Hematite, Fracture Filling, Moderate 328.00-335.80: Hematite, Pervasive, Weak 328.00-347.80: Sericite, Fracture Filling, Weak 335.80-347.90: Chlorite, Fracture Filling, Moderate STRONGER CHLORITE COMPONENT TO FRACTURES/BRECCIA ZONES 335.80-347.90: Hematite, Fracture Filling, Strong 335.80-347.90: Hematite, Pervasive, Moderate Mineralization: 335.80-347.90: Pyrite, Fracture Filling, 2-4% PYRITE NOW FOUND WITHIN CHLORITE/HEMATITE FRACUTRES Structure: 328.00-347.90: Banded 328.00-347.90: Medium Grained 328.00-347.90: Bedded 336.70-347.90: Fractured STRONGLY FRACTURED TO BRECCIATED 340.10-340.80: Brecciated 340.10-341.60: Broken Core 347.90 348.20 IMD, Mafic dykes NARROW ARCHEAN MAFIC DYKE. STRONGLY FOLIATED AND COMPRISED OF CHLORITE, AMPHIBOLE AND K-FELDSPAR. Page 5 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology 347.90-348.20: Chlorite, Pervasive, Strong Mineralization: 347.90-348.20: Pyrite, Fracture Filling, 1-2% Structure: 347.90-347.90: Contact 347.90-348.20: Foliation 348.20-348.20: Contact 347.90-348.20: Medium Grained 347.90-348.20: Foliated Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 348.20 378.40 MQZT, Mafic metasediment QUETICO METASEDIMENTS. BEDDED TO 369m THEN WEAK GNEISSIC BANDING OBSERVED. MAROON COLOUR DUE TO STRONG PERVASSIVE AND FRACTURE CONTROLLED HEMATITE ALTERATION. FROM 358.1m FRACTURES SHOW A BLEACHED CORONA WITH HEMATITE STAINING PUSHED FURTHER FROM CORE OF FRACTURE (SERICITE OR POTASSIC ALTERATION?). PORPHYROBLASTIC KYANITE? FROM 367.2-369.2m. 348.20-378.40: Chlorite, Fracture Filling, Moderate 348.20-378.40: Hematite, Fracture Filling, Strong 348.20-378.40: Hematite, Pervasive, Moderate Mineralization: 348.20-378.40: Pyrite, Fracture Filling, 1-2% Structure: 356.00-356.00: Banded 348.20-352.50: Fractured STRONGLY FRACTURED 348.20-369.00: Bedded 348.20-378.40: Medium Grained 367.20-369.20: Porphyroblastic COARSE GRAINED, BLUE/GREY KYANITE CRYSTALS 369.00-378.40: Banded 378.40 379.30 IMD, Mafic dykes ARCHEAN MAFIC DYKE. GREY-GREEN COLOUR. BRECCIATED LOWER CONTACT. AMPHIBOLE, CHLORITE WITH MINOR FELDSPAR. PYRITE ALONG FRACTURE SURFACES. 378.40-379.30: Chlorite, Pervasive, Strong 378.40-379.30: Epidote, Pervasive, Moderate Page 6 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology Mineralization: 378.40-379.30: Pyrite, Fracture Filling, 2% Structure: 378.40-378.40: Contact 379.30-379.30: Cleavage 378.40-379.30: Medium Grained 379.10-379.30: Brecciated Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 379.30 393.90 MQZT, Mafic metasediment QUETICO METASEDIMENTS. DEEP RED COULOUR WITH ABUNDANT FRACTURES, FOCUSSING HEMATITE AND CHLORITE ALTERATION. FORM 384m ABUNDANT FRACTURES, ALL ROUGHLY PERPENDICULAR TO CORE AXIS ARE OBSERVED. THESE FRACTURES SHOW STRONG HEMATITE, CHLORITE AND CARBONATE ALTERATION AND OFTEN HAVE OPEN SPACES. LOWER CONTACT WITH GABBRO BRECCIA IS GRADATIONAL OVER 20cm AS SEDIMENTS APPEAR TO BECOME DIGESTED BY UNDERLYING GABBRO. 379.30-393.90: Hematite, Pervasive, Moderate 379.30-393.90: Chlorite, Fracture Filling, Moderate 379.30-393.90: Hematite, Fracture Filling, Strong 384.00-393.90: Carbonate, Fracture Filling, Moderate Mineralization: 379.30-393.90: Pyrite, Fracture Filling, 2-4% Structure: 387.00-387.00: Banded 379.30-393.90: Fractured 379.30-393.90: Medium Grained 379.30-393.90: Banded 393.90 402.00 IGBX, Gabbro Breccia DEEP RED GABBROIC BRECCIA. DIFFUSE CONTACT WITH OVERLYING BRECCIATED QUETICO METASEDIMENTS. FROM 393.9-394.8m QUARTZ AND METASEDIMENTARY XENOLITHS COMRPISE 40% OF THE UNIT, WITH A DEEP RED FINE GRAINED GABBROIC MATRIX. FROM 394.8-402m THE GROUNDMASS IS COMPRISED OF MEDIUM GRAINED EUHEDRAL PLAGIOCLASE WHICH HAS BEEN STRONGLY HEMATIZED OR SERICITIZED AS IS OBSERVED IN UPPER SERIES GABBRO. XENOLITHS ARE LESS ABUNDANT, OCCURING AT DISCREET HORIZONS AS INDICATED IN TEXTURE LOG. LOWER CONTACT MARKED AT LAST OCCURENCE OF XENOLITHS. 1-2% DISSEMINATED PY THROUGHOUT. 393.90-402.00: Hematite, Pervasive, Strong 394.90-402.00: Sericite, Pervasive, Moderate ALTERS PLAGIOCLASE TO GREEN COLOUR Page 7 of 20 Feb 13, 2015

Hole Number: SL-14-008 From Mineralization: To Lithology 393.90-402.00: Pyrite, Disseminated, 1-2% 393.90-394.80: Xenolithic QUARTZ AND SEDIMENT XENOLITHS COMPRISE UP TO 40% THROUGH THIS INTERVAL. 393.90-394.90: Fine Grained Matrix 394.80-396.80: Massive 394.90-402.00: Medium Grained Matrix MATRIX TO XENOLITHS IS COMPRISED OF PLAGIOCLASE CUMULATE LEUCOGABBRO/MONZOGABBRO 396.80-396.90: Xenolithic QUARTZ AND PARTLY DIGESTED SEDIMENTS 396.90-397.50: Massive 397.50-399.60: Varitextured 397.50-399.60: Xenolithic QUARTZ AND SEDIMENT XENOLITHS 399.60-400.60: Mesocumulate CUMULATE PLAGIOCLASE AS IN UPPER SERIES GABBRO 400.60-402.00: Xenolithic QUARTZ, CARBONATE AND SEDIMENT XENOLITHS 400.60-402.00: Varitextured Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 402.00 600.00 IGUS, Upper Series Gabbro J591334 597.00 598.50 1.50 104.000 163.000 40.000 0.117 0.011 0.016 0.500 J591335 598.50 600.00 1.50 142.000 131.000 46.000 0.254 0.094 0.013 0.500 J591334 597.00 598.50 1.50 104.000 163.000 40.000 0.117 0.011 0.016 0.500 J591335 598.50 600.00 1.50 142.000 131.000 46.000 0.254 0.094 0.013 0.500 Page 8 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology MINOR INTERVALS: 402.00-526.00 : ILGB Leucogabbro DEEP RED MONZOGABBRO/LEUCOGABBRO. MEDIUM TO COARSE GRAINED PRISMATIC AND ACICULAR AMPHIBOLE ALONG WITH EUHEDRAL LATHS OF SERICITZED PLAGIOCLASE COMPRISE THE CUMULATE MINERALOGY. INTERCUMULUS GROUNDMASS IS STRONGLY HEMATIZED, FINE GRAINED AND ANHEDRAL. RED PODS/PATCHES OF ANHEDRAL HEMATIZED GROUND MASS FOUND THROUGHOUT UNIT, GIVING IT A SPOTTED APPEARANCE. AMPHIBOLE SHOWS GLOMERPORPHYRITIC TEXTURE FROM 416.7m-424.2m. FROM 418.5m-465m SUBANGULAR CARBONATE/CLORITE XENOLITHS APPEAR BECOMING MORE ABUNDANT DOWHOLE AND FORM UP TO 15% OF THE MODAL MINERALOGY FROM 447.1-497m. IN THIS ZONE THE CORE IS EXTREMELY VUGGY AND POROUS, AS CHLORITE AND CARBONATE RICH XENOLITHS ARE OBSERVED TO BE PARTIALLY OR COMPLETELY DISSOLVED. VUGS ALSO SHOW SELF TERMINATING QUARTZ CRYSTALS (OPEN SPACE FILLING). FROM 497-504m UNIT IS MEDIUM GRAINED WITH ABUNDANT VUGS BUT XENOLITHS ARE NEARLY ABSENT. BY 513m VUGS ARE NEARLY ABSENT, HEMATITE ALTERATION WEAKENS AND WEAK EPIDOTE ALTERATION IS OBSERVED. PLAGIOCLASE CHANGES FROM RED TO A WHITE/GREEN COLOUR (SERICITE). FROM 523.9-525m A SHARP CHANGE BACK TO DEEP RED, MEDIUM GRAINED, VUGGY MONZOGABBRO APPEARS TO BE A DYKE. ENTIRE UNIT IS STRONGLY MAGNETIC WITH 1-2% DISSEMINATED PYRITE THROUGHOUT. 526.00-600.00 : IGB Gabbro GREY-GREEN-RED GABBRO/OXIDE GABBRO. UNIT IS MARKED BY THE CHANGE IN ALTERATION ON PLAGIOCLASE, FROM DEEP RED HEMATITE TO DOMINANTLY GREEN SERICITIC ALTERATION. NARROW HEMATITE ALTERATION HALOS SURROUND PLAGIOCLASE. MORE MAFIC THAN OVERLYING MONZOGABBRO. HERE THERE IS APPROXIMATELY 30-40% AMPHIBOLE/PYROXENE WITH 60-70% PLAGIOCLASE AND 5% MAGNETITE. COARSE GRAINED THROUGHOUT BUT FINES SLIGHTLY AS LOWER CONTACT IS APPROACHED. NARROW 5-10cm WIDE RED, HEMATITE RICH VEINS/PODS CUT UNIT THROUGHOUT. WEAK IGNEOUS FOLIATION FROM 570-588m. 1-3% DISSEMINATED PY-PO MINERALIZATION THROUGHOUT. Minor 402.00-513.00: Hematite, Pervasive, Strong 447.10-526.00: Carbonate, Pervasive, Moderate 447.10-526.00: Chlorite, Patchy, Moderate 513.00-523.90: Hematite, Pervasive, Moderate 513.00-523.90: Epidote, Spots, Moderate 513.00-523.90: Sericite, Pervasive, Weak 523.90-525.00: Hematite, Pervasive, Strong 525.00-526.00: Sericite, Pervasive, Moderate 525.00-526.00: Hematite, Pervasive, Weak 525.00-526.00: Epidote, Spots, Moderate 526.00-576.00: Hematite, Pervasive, Moderate 526.00-580.00: Sericite, Pervasive, Moderate 526.00-600.00: Epidote, Spots, Moderate 576.00-600.00: Hematite, Pervasive, Weak 580.00-583.40: Sericite, Pervasive, Strong BRIGHT GREEN ALTERATION ON PLAGIOCLASE 583.40-600.00: Sericite, Pervasive, Moderate Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 9 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology Minor Mineralization: 402.00-526.00: Pyrite, Disseminated, 1-2% EUHEDRAL PYRITE Minor Structure: 514.00-526.00: Foliation WEAK IGNEOUS FOLIATION 570.00-600.00: Foliation IGNEOUS FOLIATION Minor 402.00-497.00: Coarse Grained Matrix 402.00-526.00: Mesocumulate CUMULATE PLAGIOCLASE AND AMPHIBOLE 416.70-424.20: Glomerophyric AMPHIBOLE AGGREGATES GIVE CORE A SPOTTED APPEARANCE 447.10-497.00: Xenolithic CARBONATE AND CHLORITE XENOLITHS UP TO 5cm WIDE 497.00-504.00: Medium Grained 503.50-523.90: Coarse Grained 514.00-523.90: Foliated IGNEOUS FOLIATION DEFINED BY AMPHIBOLE AND PLAGIOCLASE ORIENTATION 523.90-525.00: Massive 525.00-526.00: Foliated IGNEOUS FOLIATION DEFINED BY AMPHIBOLE AND PLAGIOCLASE ORIENTATION 526.00-600.00: Coarse Grained 526.00-600.00: Mesocumulate PLAGIOCLASE-PYROXENE/AMPHIBOLE CUMULATE 570.00-600.00: Foliated IGNEOUS FOLIATION DEFINED BY PLAGIOCLASE ORIENTATION Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct 600.00 655.60 IGLS, Lower Series Gabbro Page 10 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct J591336 600.00 601.50 1.50 182.000 166.000 53.000 0.290 0.150 0.018 0.500 J591336 600.00 601.50 1.50 182.000 166.000 53.000 0.290 0.150 0.018 0.500 J591337 601.50 603.00 1.50 174.000 77.000 56.000 0.082 0.096 0.002 0.500 J591337 601.50 603.00 1.50 174.000 77.000 56.000 0.082 0.096 0.002 0.500 J591338 603.00 604.50 1.50 178.000 113.000 59.000 0.027 0.045 0.002 0.500 J591338 603.00 604.50 1.50 178.000 113.000 59.000 0.027 0.045 0.002 0.500 J591339 604.50 606.00 1.50 171.000 134.000 57.000 0.018 0.044 0.003 0.500 J591339 604.50 606.00 1.50 171.000 134.000 57.000 0.018 0.044 0.003 0.500 J591341 606.00 607.50 1.50 239.000 110.000 67.000 0.019 0.023 0.002 0.500 J591342 607.50 609.00 1.50 290.000 99.000 78.000 0.015 0.008 0.001 0.500 J591343 609.00 610.50 1.50 273.000 77.000 75.000 0.018 0.006 0.004 0.500 J591344 610.50 612.00 1.50 279.000 109.000 75.000 0.018 0.013 0.002 0.500 J591345 612.00 613.50 1.50 289.000 61.000 78.000 0.016 0.005 0.001 0.500 J591346 613.50 615.00 1.50 299.000 53.000 83.000 0.028 0.009 0.002 0.500 J591347 615.00 616.50 1.50 317.000 69.000 86.000 0.022 0.009 0.003 0.500 J591348 616.50 618.00 1.50 404.000 78.000 91.000 0.034 0.012 0.002 0.500 J591349 618.00 619.50 1.50 535.000 135.000 102.000 0.042 0.029 0.003 0.500 J591351 619.50 621.00 1.50 570.000 100.000 107.000 0.035 0.017 0.002 0.500 J591352 621.00 622.50 1.50 603.000 105.000 111.000 0.054 0.048 0.003 0.500 J591353 622.50 624.00 1.50 607.000 166.000 111.000 0.053 0.038 0.007 0.500 J591354 624.00 625.50 1.50 578.000 100.000 111.000 0.025 0.010 0.002 0.500 J591355 625.50 627.00 1.50 546.000 126.000 105.000 0.045 0.029 0.004 0.500 J591356 627.00 628.50 1.50 513.000 91.000 101.000 0.024 0.015 0.002 0.500 J591357 628.50 630.00 1.50 485.000 99.000 93.000 0.036 0.026 0.002 0.500 J591358 630.00 631.50 1.50 474.000 113.000 96.000 0.024 0.025 0.002 0.500 J591359 631.50 633.00 1.50 438.000 90.000 93.000 0.021 0.014 0.001 0.500 J591361 633.00 634.50 1.50 273.000 96.000 72.000 0.013 0.006 0.002 0.500 J591362 634.50 636.00 1.50 232.000 110.000 70.000 0.014 0.006 0.005 0.500 J591363 636.00 637.50 1.50 231.000 100.000 72.000 0.020 0.005 0.002 0.500 J591364 637.50 639.00 1.50 208.000 86.000 69.000 0.029 0.005 0.002 0.500 J591365 639.00 640.50 1.50 220.000 106.000 69.000 0.020 0.005 0.002 0.500 J591366 640.50 642.00 1.50 219.000 95.000 62.000 0.022 0.022 0.003 0.500 J591367 642.00 643.50 1.50 208.000 110.000 66.000 0.023 0.007 0.002 0.500 J591368 643.50 645.00 1.50 204.000 132.000 67.000 0.027 0.011 0.004 0.500 J591369 645.00 646.50 1.50 215.000 195.000 67.000 0.022 0.019 0.002 0.500 J591370 645.00 646.50 1.50 218.000 216.000 68.000 0.026 0.031 0.003 0.500 J591371 646.50 648.00 1.50 191.000 116.000 66.000 0.024 0.006 0.002 0.500 J591372 648.00 649.00 1.00 195.000 125.000 64.000 0.019 0.003 0.002 0.500 J591373 649.00 650.00 1.00 188.000 103.000 68.000 0.026 0.005 0.001 0.500 J591374 650.00 651.00 1.00 207.000 81.000 67.000 0.014 0.005 0.023 0.500 J591375 651.00 652.00 1.00 214.000 55.000 67.000 0.010 0.003 0.002 0.500 J591376 652.00 653.00 1.00 224.000 84.000 69.000 0.013 0.006 0.001 0.500 J591377 653.00 654.00 1.00 234.000 69.000 69.000 0.007 0.004 0.001 0.500 J591378 654.00 655.00 1.00 268.000 206.000 73.000 0.018 0.075 0.020 0.500 J591379 655.00 655.60 0.60 288.000 394.000 74.000 0.068 0.113 0.009 0.500 J591342 607.50 609.00 1.50 290.000 99.000 78.000 0.015 0.008 0.001 0.500 Page 11 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct J591343 609.00 610.50 1.50 273.000 77.000 75.000 0.018 0.006 0.004 0.500 J591344 610.50 612.00 1.50 279.000 109.000 75.000 0.018 0.013 0.002 0.500 J591345 612.00 613.50 1.50 289.000 61.000 78.000 0.016 0.005 0.001 0.500 J591346 613.50 615.00 1.50 299.000 53.000 83.000 0.028 0.009 0.002 0.500 J591347 615.00 616.50 1.50 317.000 69.000 86.000 0.022 0.009 0.003 0.500 J591348 616.50 618.00 1.50 404.000 78.000 91.000 0.034 0.012 0.002 0.500 J591349 618.00 619.50 1.50 535.000 135.000 102.000 0.042 0.029 0.003 0.500 J591351 619.50 621.00 1.50 570.000 100.000 107.000 0.035 0.017 0.002 0.500 J591352 621.00 622.50 1.50 603.000 105.000 111.000 0.054 0.048 0.003 0.500 J591353 622.50 624.00 1.50 607.000 166.000 111.000 0.053 0.038 0.007 0.500 J591354 624.00 625.50 1.50 578.000 100.000 111.000 0.025 0.010 0.002 0.500 J591355 625.50 627.00 1.50 546.000 126.000 105.000 0.045 0.029 0.004 0.500 J591356 627.00 628.50 1.50 513.000 91.000 101.000 0.024 0.015 0.002 0.500 J591357 628.50 630.00 1.50 485.000 99.000 93.000 0.036 0.026 0.002 0.500 J591358 630.00 631.50 1.50 474.000 113.000 96.000 0.024 0.025 0.002 0.500 J591359 631.50 633.00 1.50 438.000 90.000 93.000 0.021 0.014 0.001 0.500 J591361 633.00 634.50 1.50 273.000 96.000 72.000 0.013 0.006 0.002 0.500 J591362 634.50 636.00 1.50 232.000 110.000 70.000 0.014 0.006 0.005 0.500 J591363 636.00 637.50 1.50 231.000 100.000 72.000 0.020 0.005 0.002 0.500 J591364 637.50 639.00 1.50 208.000 86.000 69.000 0.029 0.005 0.002 0.500 J591365 639.00 640.50 1.50 220.000 106.000 69.000 0.020 0.005 0.002 0.500 J591366 640.50 642.00 1.50 219.000 95.000 62.000 0.022 0.022 0.003 0.500 J591367 642.00 643.50 1.50 208.000 110.000 66.000 0.023 0.007 0.002 0.500 J591368 643.50 645.00 1.50 204.000 132.000 67.000 0.027 0.011 0.004 0.500 J591369 645.00 646.50 1.50 215.000 195.000 67.000 0.022 0.019 0.002 0.500 J591370 645.00 646.50 1.50 218.000 216.000 68.000 0.026 0.031 0.003 0.500 J591371 646.50 648.00 1.50 191.000 116.000 66.000 0.024 0.006 0.002 0.500 J591372 648.00 649.00 1.00 195.000 125.000 64.000 0.019 0.003 0.002 0.500 J591373 649.00 650.00 1.00 188.000 103.000 68.000 0.026 0.005 0.001 0.500 J591374 650.00 651.00 1.00 207.000 81.000 67.000 0.014 0.005 0.023 0.500 J591375 651.00 652.00 1.00 214.000 55.000 67.000 0.010 0.003 0.002 0.500 J591376 652.00 653.00 1.00 224.000 84.000 69.000 0.013 0.006 0.001 0.500 J591377 653.00 654.00 1.00 234.000 69.000 69.000 0.007 0.004 0.001 0.500 J591378 654.00 655.00 1.00 268.000 206.000 73.000 0.018 0.075 0.020 0.500 J591379 655.00 655.60 0.60 288.000 394.000 74.000 0.068 0.113 0.009 0.500 Page 12 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology MINOR INTERVALS: 600.00-606.40 : IGB Gabbro CONTACT WITH OVERLYING UPPER SERIES GABBRO MARKED BY ABSENCE OF CUMULATE LATHS OF PLAGIOCLASE. 55% PYROXENE, 45% PLAGIOCLASE, 5% MAGNETITE. OPHITIC TO GRANULAR TEXTURE WITH EUHEDRAL PYROXENE SURROUNDED BY WHITE PLAGIOCLASE. WEAK HEMATITE ALTERATION ALTERS FELDSPAR AND GROUNDMASS. 1-2% DISSEMINATED PY-PO. 606.40-633.00 : IOMGB Olivine Melagabbro GRADUAL FRACTIONATION OF OVERLYING GABBRO TO A MORE MAFIC COMPOSITION WITH OLIVINE. WEAK OIKOCRYSTIC TEXTURE WITH PLAGIOCLASE SURROUNDING PYROXENE AND OLIVINE CHADACRYSTS. ALTERED PYROXENE PHENOCRYTS FROM 606.4-613m MOTTLED APPEARANCE, ESPECIALLY FROM 618-629m. 50-65% PYROXENE, 10-20% PLAGIOCLASE 5-15% OLIVINE, 5% BIOTITE. CHLORITIC VEIN AT 627m SHOWS SLICKENLINES AND MAY REPRESENT A FAULT BUT THERE IS NO SIGNIFICANT CHANGE IN LITHOLOGY ON EITHER SIDE. 633.00-655.60 : IGB Gabbro GRADUAL FINING OF OVERLYING OLIVINE MELAGABBRO TO A FINE GRAINED, MASSIVE GABBRO. VERY MONOTONOUS UNIT COMPRISED OF 45-55% PYROXENE, 40-50% PLAGIOCLASE, 0-10% OLIVINE AND TRACE BIOTITE. PLAGIOCLASE OIKOCRYSTS ENCLOSE MAFIC PHASES. MINOR SULFIDE MINERALIZATION OCCURS AS COARSE, SINGLE BLEBS OF CPY RICH SULFIDE. BLEB AT 645m, AND FROM 654.7-655.6m 3 COARSE GRAINED BLEBS OF CPY WITH MINOR PO AND BORNITE? (STRONGLY TARNISHED INCLUSION IN CPY) Minor 618.00-633.00: Chlorite, Pervasive, Weak 627.00-627.00: Chlorite, Veins, Strong POSSIBLE FAULT? Minor Mineralization: 600.00-606.40: Pyrrhotite/Pyrite, Disseminated, 1-2% 654.70-655.60: Pyrrhotite/Chalcopyrite, Blebby, 1% 3 ISOLATED BLEBS OF CPY RICH FRACTIONATED SULFIDE Minor Structure: 606.40-633.00: Slikensides CHLORITIC VEIN Minor 600.00-606.40: Ophitic 600.00-606.40: Fine Grained - Medium Grained 606.40-613.00: Medium Grained 606.40-613.00: Pyroxene Phyric 606.40-633.00: Oikocrysts WEAKLY OIKOCRYSTIC. PLAGIOCLASE IS OIKOCRYSTIC PHASE. 613.00-633.00: Fine Grained 633.00-655.60: Oikocrysts PLAGIOCLASE OIKOCRYSTS ENCLOSE PYROXENE AND OLIVINE CHADACRYSTS 633.00-655.60: Massive 633.00-655.60: Fine Grained Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 13 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology 655.60 678.80 IUMS, Ultramafic Series Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 14 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct J591380 655.60 656.60 1.00 683.000 680.000 126.000 0.128 0.113 0.014 0.500 J591380 655.60 656.60 1.00 683.000 680.000 126.000 0.128 0.113 0.014 0.500 J591381 656.60 657.60 1.00 935.000 1,510.000 130.000 1.190 0.730 0.080 0.700 J591381 656.60 657.60 1.00 935.000 1,510.000 130.000 1.190 0.730 0.080 0.700 J591383 657.60 658.60 1.00 1,215.000 2,500.000 122.000 1.520 0.889 0.111 1.400 J591383 657.60 658.60 1.00 1,215.000 2,500.000 122.000 1.520 0.889 0.111 1.400 J591384 658.60 659.60 1.00 1,505.000 3,130.000 140.000 1.605 0.897 0.132 1.900 J591384 658.60 659.60 1.00 1,505.000 3,130.000 140.000 1.605 0.897 0.132 1.900 J591385 659.60 660.60 1.00 1,785.000 5,190.000 132.000 2.200 1.360 0.142 3.200 J591385 659.60 660.60 1.00 1,785.000 5,190.000 132.000 2.200 1.360 0.142 3.200 J591386 660.60 661.60 1.00 1,635.000 4,730.000 124.000 2.070 1.310 0.116 2.500 J591386 660.60 661.60 1.00 1,635.000 4,730.000 124.000 2.070 1.310 0.116 2.500 J591387 661.60 662.60 1.00 2,170.000 6,480.000 147.000 4.030 2.370 0.201 3.800 J591388 662.60 663.60 1.00 1,115.000 2,380.000 114.000 1.290 0.802 0.083 1.400 J591389 663.60 664.60 1.00 1,070.000 2,080.000 120.000 0.994 0.566 0.078 0.900 J591391 664.60 665.40 0.80 1,055.000 2,300.000 115.000 0.742 0.477 0.062 1.600 J591392 665.40 666.40 1.00 498.000 876.000 69.000 0.131 0.089 0.013 0.800 J591393 666.40 667.40 1.00 444.000 582.000 68.000 0.048 0.029 0.005 0.500 J591394 667.40 668.40 1.00 815.000 1,695.000 103.000 0.635 0.364 0.042 0.900 J591395 668.40 669.40 1.00 563.000 796.000 83.000 0.134 0.088 0.013 0.500 J591396 669.40 670.40 1.00 1,240.000 3,120.000 128.000 1.130 0.699 0.072 1.700 J591397 670.40 671.40 1.00 1,555.000 4,020.000 149.000 1.290 0.797 0.086 2.600 J591398 671.40 672.40 1.00 836.000 1,390.000 122.000 0.481 0.287 0.034 1.000 J591399 672.40 673.40 1.00 879.000 2,200.000 103.000 0.628 0.373 0.045 1.700 J591401 673.40 674.40 1.00 1,095.000 2,950.000 124.000 0.827 0.512 0.056 1.900 J591402 674.40 675.40 1.00 509.000 878.000 88.000 0.141 0.094 0.013 0.700 J591403 675.40 676.40 1.00 482.000 767.000 74.000 0.056 0.033 0.009 0.700 J591404 676.40 676.90 0.50 513.000 870.000 98.000 0.277 0.169 0.019 0.800 J591405 676.90 677.90 1.00 295.000 375.000 66.000 0.040 0.024 0.004 0.500 J591406 677.90 678.80 0.90 461.000 844.000 74.000 0.309 0.187 0.021 0.700 J591388 662.60 663.60 1.00 1,115.000 2,380.000 114.000 1.290 0.802 0.083 1.400 J591389 663.60 664.60 1.00 1,070.000 2,080.000 120.000 0.994 0.566 0.078 0.900 J591392 665.40 666.40 1.00 498.000 876.000 69.000 0.131 0.089 0.013 0.800 J591393 666.40 667.40 1.00 444.000 582.000 68.000 0.048 0.029 0.005 0.500 J591394 667.40 668.40 1.00 815.000 1,695.000 103.000 0.635 0.364 0.042 0.900 J591395 668.40 669.40 1.00 563.000 796.000 83.000 0.134 0.088 0.013 0.500 J591396 669.40 670.40 1.00 1,240.000 3,120.000 128.000 1.130 0.699 0.072 1.700 J591397 670.40 671.40 1.00 1,555.000 4,020.000 149.000 1.290 0.797 0.086 2.600 J591398 671.40 672.40 1.00 836.000 1,390.000 122.000 0.481 0.287 0.034 1.000 J591399 672.40 673.40 1.00 879.000 2,200.000 103.000 0.628 0.373 0.045 1.700 J591401 673.40 674.40 1.00 1,095.000 2,950.000 124.000 0.827 0.512 0.056 1.900 J591402 674.40 675.40 1.00 509.000 878.000 88.000 0.141 0.094 0.013 0.700 J591403 675.40 676.40 1.00 482.000 767.000 74.000 0.056 0.033 0.009 0.700 J591404 676.40 676.90 0.50 513.000 870.000 98.000 0.277 0.169 0.019 0.800 J591405 676.90 677.90 1.00 295.000 375.000 66.000 0.040 0.024 0.004 0.500 J591406 677.90 678.80 0.90 461.000 844.000 74.000 0.309 0.187 0.021 0.700 Page 15 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct MINOR INTERVALS: 655.60-662.40 : IOMGB Olivine Melagabbro SHARP CONTACT WITH OVERLYING GABBRO MARKED BY COARSER GRAIN SIZE (MEDIUM GRAINED), WEAK TO MODERATE SERPENTINE VEINING AND PRESENCE OF CHLORITE/CARBONATE CLOTS/XENOLITHS. UNIT IS VARIABLY TEXTURED AND HETEROGENOUS WITH RAPID CHANGES. FINELY DISSEMINATED SULFIDES THROUGHOUT UNIT, CONSISTING OF CPY-PO-PY WITH VISIBLE MAGNETITE IN COARSER BLEBS. APPROXIMATELY 2-3% AVERAGE SULFIDE THROUGHOUT UNIT WITH DISTRIBUTION INDICATED IN MINERALIZATION LOG. 662.40-665.30 : IPDT IPDT COARSE GRAINED OLIVINE MESOCUMULATE PERIDOTITE. EUHEDRAL/SKELETAL OLIVINE ARE UP TO 5mm IN DIAMETER, GREY-WHITE IN COLOUR, AND COMPRISE 40-60% OF THE MODAL MINERALOGY. INTERCUMULUS MATERIAL IS ANHEDRAL, AND APPEARS TO BE CHLORITIZED/SERPENTINIZED RELICT PYROXENE (30-50%). UNIT AVERAGES 5% COARSE GRAINED, BLEBBY AND FINELY DISSEMINATED CPY-PO MINERALIZATION. LOWER CONTACT MARKED BY STRONGLY CHLORITE/AMPHIBOLE ALTERED MOTTLED ZONE WHICH TRANSITIONS INTO UNDERLYING GABBROIC UNIT. 665.30-676.90 : IMGB Melagabbro VARIABLY TEXTURED UNIT OVERALL WITH ROCK TYPES RANGING FROM GABBRO TO OLIVINE MELAGABBRO. FROM 665.3-667.6m CORE IS GABBROIC IN COMPOSITION, FRACTIONATING DOWNWARDS TO OLIVINE MELAGABBRO. INTERVAL IS CHARACTERIZED BY MODERATE TO STRONG CARBONATE ALTERATION OCCURING PERVASSIVELY AND IN FRACTURE CONTROLED VEINS. COARSE GRAINED CHLORITE PODS FOUND THROUGHOUT. TRACE PO THROUGH THIS INTERVAL. FROM 667.6-667.9m THE UNIT CHANGES TO A COARSE GRAINED, VARITEXTURED GABBRO WITH 5% COARSE GRAINED BLEBS OF PO-CPY WHICH ARE FOUND WITHIN AND ADJACENT TO CHLORITE/QUARTZ PODS. FROM 667.9-668.4m OLIVINE CUMULATE TEXTURE NOTED WHICH FINES AND FRACTIONATES DOWNWARDS. FROM 668.4-669.7m FINE GRAINED MELAGABBRO WITH CHLORITE PODS AND 1-2% FINELY DISSEMINATED PO-CPY. FROM 669.7-670.7m VARITEXTURED WITH 5% COARSE GRAINED BLEBBY PO-CPY-PN? SULFIDES SHOW BRIGHT PINK PO ALONGSIDE CPY AND A QUICKLY TARNISHING SULFIDE PHASE. FROM 670.7-676.9m UNIT IS FAIRLY MASSIVE, MEDIUM TO FINE GRAINED WITH ONLY MINOR PATCHES OF VARITEXTURED GABBRO. FROM 670.7-672.4m UNIT CONTAINS 3-4% FINELY DISSEMINATED PO-CPY MINERALIZATION, WHILE FROM 672.4-673.6m SULFIDES ARE FOUND AS MEDIUM TO COARSE GRAINED BLEBS ASSOCIATED WITH CHLORITE/QUARTZ PODS (3-4%). FROM 673.6-675.9m UNIT IS FAIRLY HOMOGENOUS, MELAGABBRO WITH 1% FINELY DISSEMINATED PO-CPY. FROM 675.9-676.7m UNIT IS VARITEXTURED WITH A COARSE POD OF ANORTHOSITIC GABBRO-DIORITE FROM 676-676.2m. FROM 676.2-676.9m UNIT FINES, WITH LOWER MOST 10cm SHOWING PYROXENE PHYRIC TEXTURE WITH MOTTLED FINE GRAINED GROUNDMASS. GRADUAL TRANSITION TO UNDERLYING GABBRO. 676.90-678.80 : IGB Gabbro MEDIUM TO FINE GRAINED, INTERGRANULAR TEXTURED GABBRO WITH MINOR LAYERING. IGNEOUS CONTACT AT 677.3m AT 55 DTCA. TRACE FINE DISSEMINATED SULFIDE TO 678.6m FROM 678.6m 5% FINELY DISSEMINATED PO-CPY MINERALIZATION TO LOWER CONTACT WITH QUETICO SEDIMENTS. BASAL CONTACT IS SHARP BUT IRREGULAR, ORIENTED AT APPROXIMATELY 30 DTCA. Page 16 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology Sample # Minor 655.60-659.90: Serpentinization, Veins, Moderate 662.40-665.30: Chlorite, Pervasive, Strong ALTERS GROUNDMASS 662.40-665.30: Serpentinization, Pervasive, Strong 665.30-667.60: Carbonate, Veins, Strong 665.30-676.90: Chlorite, Pods, Moderate PODS/XENOLITHS OF CHLORITE THROUGHOUT Minor Mineralization: 655.60-659.40: Pyrrhotite/Chalcopyrite, Disseminated, 2% 659.40-659.90: Pyrrhotite/Chalcopyrite, Blebby, 5% 659.40-662.40: Pyrrhotite/Pyrite/Chalcopyrite, Disseminated, 5% 662.40-665.30: Pyrrhotite/Chalcopyrite, Blebby, 5% BLEBS OF SULFIDE ARE FRACTIONATED AND MAY CONTAIN PENTLANDITE. OCCUR INTERSTITIA 665.30-667.60: Pyrrhotite, Trace, TRACE% 667.60-667.90: Pyrrhotite/Chalcopyrite, Blebby, 5% 667.60-668.40: Pyrrhotite/Chalcopyrite, Trace, TRACE% 668.40-669.70: Pyrrhotite/Chalcopyrite, Disseminated, 1-2% 669.70-670.70: Pyrrhotite/Pentlandite/Chalcopyrite, Blebby, 5% 670.70-672.40: Pyrrhotite/Chalcopyrite, Disseminated, 3-4% 672.40-673.60: Pyrrhotite/Chalcopyrite, Blebby, 3-4% 673.60-675.90: Pyrrhotite/Chalcopyrite, Disseminated, 1% 675.90-676.90: Pyrrhotite/Chalcopyrite, Blebby, 3% 676.90-678.60: Pyrrhotite/Chalcopyrite, Disseminated, TRACE% 678.60-678.80: Pyrrhotite/Chalcopyrite, Disseminated, 5% Minor Structure: 655.60-658.50: Veins SERPENTINE VEINS 677.30-677.30: Contact IGNEOUS LAYER 678.80-678.80: Contact BASAL CONTACT From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 17 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Minor Lithology 655.60-658.50: Medium Grained 658.50-659.10: Fine Grained 659.10-659.90: Varitextured 659.90-662.40: Pyroxene Phyric FINE GRAINED, CHLORITIZED PHENOCRYSTS OF PYROXENE VISIBLE THROUGHOUT 659.90-662.40: Medium Grained 662.40-665.20: Mesocumulate OLIVINE CUMULATE TEXTURE. INTERCUMULUS PHASES ARE STRONGLY CHLORITE/SERPENTINE 662.40-665.30: Coarse Grained 665.20-665.30: Varitextured MOTTLED, ANHEDRAL TRANSITION ZONE TO UNDERLYING GABBRO 665.30-667.60: Massive 665.30-667.60: Medium Grained 667.60-667.90: Varitextured 667.90-668.40: Mesocumulate OLIVINE CUMULATE LAYER 667.90-668.40: Medium Grained - Coarse Grained 668.40-669.70: Fine Grained - Medium Grained 669.70-670.70: Varitextured 670.70-676.90: Massive 670.70-676.90: Medium Grained - Fine Grained 675.90-676.70: Varitextured LEUCOCRATIC PODS/VEINS 676.70-676.90: Pyroxene Phyric 676.90-678.80: Massive INTERGRANULAR TEXTURE 676.90-678.80: Fine Grained - Medium Grained 678.80 714.00 MQZT, Mafic metasediment Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct Page 18 of 20 Feb 13, 2015

Hole Number: SL-14-008 From To Lithology FOOTWALL QUETICO METASEDIMENTS. THERMALLY ALTERED THROUGH TO BOTTOM OF HOLE. FROM 678.8-687.8m ENTIRE UNIT LOOKS BRECCIATED/PARTIALLY MELTED WITH LEUCOCRATIC AND CHLORITIC VEINS/PODS CROSS CUTTTING UNIT. IN CONTRAST TO OVERLYING BRECCIAS WHICH EXHIBIT BRITTLE DEFORMATION AND LATER HYDROTHERMAL ALTERATION, THIS UNIT LOOKS TO BE HYDRALICALLY BRECCIATED/MELTED. VEINS/PODS OFTEN CONTAIN BLEBBY TO DISSEMINATED CPY-PO MINERALIZATION. THIS INTERVAL AVERAGES 2% PO-CPY MINERALIZATION THROUGHOUT. COARSE GRAINED SULFIDE AT 680m SHOWS BRIGHT PINK PO-PN? WITH FRACTIONATED CPY AROUND OUTSIDE. FROM 687.8-714m UNIT APPEARS BLEACHED TO A GREY-GREEN COLOUR RELATIVE AND SHOWS MINOR BRECCIATION OF HAS ABUNDANT CROSS CUTTING, PINK-WHITE FELSIC VEINLETS, WHICH ARE NOT TYPICAL TO OVERLYING HANGING WALL SEDIMENTS. Sample # From To Length Ni ppm Cu ppm Co ppm Pt ppm Pd ppm Au ppm Ag ppm S pct J591407 678.80 679.80 1.00 303.000 499.000 59.000 0.084 0.050 0.008 0.500 J591408 679.80 680.80 1.00 520.000 531.000 67.000 0.223 0.160 0.009 0.500 J591409 680.80 681.80 1.00 326.000 231.000 66.000 0.005 0.007 0.001 0.500 J591410 680.80 681.80 1.00 322.000 236.000 67.000 0.005 0.007 0.001 0.500 J591411 681.80 682.80 1.00 239.000 136.000 51.000 0.005 0.005 0.001 0.500 J591412 682.80 683.80 1.00 188.000 107.000 43.000 0.005 0.004 0.001 0.500 J591413 683.80 684.80 1.00 246.000 177.000 53.000 0.005 0.006 0.001 0.500 J591414 684.80 685.80 1.00 218.000 516.000 44.000 0.086 0.056 0.008 0.600 J591415 685.80 686.80 1.00 184.000 179.000 40.000 0.038 0.030 0.002 0.500 J591416 686.80 687.80 1.00 163.000 91.000 36.000 0.005 0.004 0.001 0.500 J591417 687.80 688.80 1.00 104.000 46.000 29.000 0.005 0.002 0.001 0.500 J591418 688.80 689.80 1.00 81.000 7.000 34.000 0.005 0.002 0.001 0.500 678.80-687.80: Chlorite, Patchy, Moderate ASSOCIATED WITH LEUCOCRATIC VEINS/PODS 687.80-714.00: K-Feldspar, Veins, Weak PINK X-CUTTING VEINS 687.80-714.00: Bleaching, Pervasive, Strong Mineralization: 678.80-687.80: Pyrrhotite/Chalcopyrite, Blebby, 2% 687.80-714.00: Pyrite, Trace, TRACE% Structure: 687.80-714.00: Banded 678.80-687.90: Brecciated 687.90-714.00: Banded Page 19 of 20 Feb 13, 2015

Hole Number: SL-14-008 Survey Data Depth Azimuth Decimal Dip Decimal Test Type Flag 0.00 290.00-85.00 REFLEX O 30.00 270.60-84.30 REFLEX N 60.00 289.70-84.10 REFLEX O 120.00 6.90-82.80 REFLEX N 180.00 287.30-81.40 REFLEX O 240.00 300.80-79.50 REFLEX O 300.00 299.20-77.70 REFLEX O 360.00 288.30-76.00 REFLEX O 420.00 279.20-74.60 REFLEX O 480.00 287.50-73.20 REFLEX O 540.00 289.10-72.30 REFLEX O 600.00 293.60-70.60 REFLEX O 660.00 309.70 70.00 REFLEX O Comments Page 20 of 20 Feb 13, 2015

Appendix B: Drill Plan and Cross Sections

SL-14-006 Collar: 333839mE, 5394604mN Az= 270 degrees, Dip=-85 degrees SL-14-008 Collar: 333839mE, 5394604mN Az= 290 degrees, Dip=-85 degrees Section Orientation: 150 degrees Looking NE Scale 1:5000 0 100 Metres 200

SL-14-007 Collar: 334330mE, 5395240mN Az= 295 degrees, Dip=-78 degrees Section Orientation: 270 degrees Looking North Scale 1:2500 0 50 Metres 100

Appendix C: Assays

2.57 0.005 0.034 0.032 135.0 34.8 1480 2.79 2.70 1.20 1.39 9.1 3.59 2.7 0.47 2.61 0.002 0.031 0.030 134.5 34.3 1380 2.77 2.77 1.19 1.31 9.3 3.77 2.8 0.45 2.65 0.002 0.022 0.012 117.5 36.9 1290 2.49 2.94 1.20 1.32 10.2 4.17 3.0 0.51 2.50 0.001 0.023 0.017 111.0 40.7 1230 2.76 3.15 1.37 1.37 11.3 4.23 3.0 0.56 2.74 0.007 0.022 0.016 99.5 31.8 1130 2.84 2.73 1.10 1.33 10.0 3.75 2.7 0.49 2.53 0.001 0.028 0.006 102.0 32.8 940 1.87 2.73 1.19 1.30 10.3 3.68 2.5 0.51 2.71 0.003 0.032 0.017 125.5 39.4 1020 1.55 3.29 1.48 1.51 11.5 4.73 3.2 0.57 2.69 0.004 0.032 0.012 151.5 43.7 970 1.57 3.32 1.49 1.56 11.5 4.77 3.6 0.61 2.77 0.004 0.039 0.015 162.5 50.6 970 1.88 3.41 1.41 1.77 12.4 4.62 4.0 0.58 0.06 0.032 0.182 0.345 1.52 0.014 0.116 0.085 156.5 50.5 1010 1.66 3.37 1.47 1.74 12.8 4.80 5.5 0.63 1.16 0.002 0.024 0.006 176.5 52.3 1050 2.04 3.47 1.55 1.75 12.9 5.04 4.3 0.61 2.74 0.002 0.022 0.016 196.0 57.1 920 1.80 3.52 1.68 1.94 13.2 5.40 4.6 0.69 1.45 0.008 0.092 0.065 192.5 56.2 840 1.42 3.52 1.60 1.86 13.5 4.93 4.6 0.64 1.36 0.001 0.017 0.004 183.5 49.6 770 1.88 3.52 1.51 1.82 12.6 4.92 4.1 0.62 2.73 0.002 0.022 0.011 180.5 51.9 870 2.16 3.60 1.60 1.85 13.1 5.18 4.1 0.67 2.81 0.002 0.028 0.021 184.0 50.8 800 2.05 3.36 1.59 1.68 13.0 4.76 4.0 0.59 1.18 <0.001 <0.005 <0.001 2.80 0.001 0.014 0.006 194.0 54.7 810 1.58 3.67 1.63 1.88 13.1 5.17 4.3 0.72 2.65 0.001 0.036 0.005 191.5 49.4 740 1.62 3.66 1.55 1.64 13.7 5.24 4.3 0.67 2.34 0.001 0.029 0.005 162.5 44.9 760 1.65 3.49 1.52 1.61 12.2 4.95 3.6 0.63 2.75 0.001 0.028 0.007 192.0 49.5 820 1.44 3.37 1.63 1.70 12.7 5.45 4.2 0.66 2.91 0.001 0.018 0.007 179.0 48.4 890 1.72 3.45 1.51 1.62 12.1 4.97 4.0 0.59 2.82 0.002 0.013 0.006 165.0 46.8 1020 1.29 3.34 1.45 1.66 11.7 4.70 3.9 0.60 2.78 0.001 0.011 0.009 167.0 46.7 1170 1.55 3.25 1.44 1.59 11.7 4.82 3.9 0.59 2.81 0.001 0.011 0.007 173.5 43.4 1290 1.45 3.06 1.33 1.49 11.1 4.21 3.4 0.52 2.79 0.001 0.018 0.012 155.0 41.6 1400 1.53 2.92 1.42 1.47 10.4 4.21 3.3 0.51 2.69 0.003 0.022 0.022 142.0 38.3 1460 1.13 2.84 1.23 1.37 9.5 3.91 3.1 0.45 2.78 0.016 0.046 0.067 137.0 35.3 1520 1.05 2.71 1.16 1.26 9.0 3.64 2.9 0.48 0.06 0.033 0.172 0.333 2.58 0.003 0.045 0.027 115.5 34.0 1690 1.36 2.53 1.24 1.24 8.9 3.72 2.7 0.46 1.09 0.012 0.116 0.097 96.4 30.4 1920 1.82 2.44 1.04 1.19 8.3 3.61 2.6 0.45 1.18 0.004 0.053 0.016 35.4 28.4 1630 3.52 1.77 0.74 0.84 6.1 2.30 2.5 0.29 2.31 0.005 0.093 0.046 95.0 26.6 2150 1.48 1.70 0.67 0.94 6.7 2.54 2.2 0.31 2.58 0.021 0.111 0.100 87.2 22.5 3040 0.96 1.56 0.58 0.75 7.1 2.13 1.7 0.26 2.49 0.016 0.059 0.047 78.4 23.4 2470 1.34 1.64 0.70 0.88 6.8 2.38 1.9 0.32 2.58 0.011 0.103 0.082 72.8 19.4 2360 1.19 1.54 0.73 0.73 5.7 2.29 1.7 0.27 2.71 0.033 0.380 0.273 50.3 20.9 2500 2.13 1.65 0.71 0.78 6.1 2.20 1.8 0.29 2.53 0.061 0.548 0.402 63.0 26.6 2240 1.99 2.01 0.85 0.88 6.5 2.67 2.3 0.34 <0.02 0.061 0.507 0.378

14.3 0.13 10.3 20.8 4.71 14.1 4.85 1 335 0.7 0.51 1.07 0.16 0.30 222 14.0 0.12 10.4 20.5 4.67 14.8 4.61 1 341 0.6 0.53 1.07 0.17 0.33 231 15.4 0.14 12.1 21.7 5.01 12.4 4.83 1 384 0.7 0.51 1.24 0.17 0.40 219 17.0 0.15 12.4 23.3 5.43 12.2 5.39 1 356 0.7 0.58 1.33 0.18 0.40 222 12.9 0.12 9.7 20.5 4.44 14.7 4.54 1 413 0.5 0.52 0.94 0.15 0.23 243 13.3 0.14 9.7 21.0 4.65 10.3 4.76 1 369 0.6 0.52 0.94 0.17 0.27 269 15.9 0.17 12.3 24.3 5.54 9.0 5.55 1 363 0.7 0.60 1.00 0.18 0.32 300 18.2 0.18 13.6 25.2 5.91 11.1 5.90 1 386 0.9 0.66 1.39 0.20 0.46 279 21.2 0.18 15.8 28.5 6.70 13.1 5.86 1 453 1.0 0.64 1.62 0.20 0.50 231 21.5 0.15 16.3 28.8 6.77 10.8 6.06 1 455 1.0 0.64 1.84 0.21 0.60 243 22.1 0.18 16.3 29.7 7.03 13.8 6.44 1 462 1.0 0.68 1.58 0.21 0.54 262 24.5 0.22 18.5 32.4 7.60 13.5 7.10 1 454 1.1 0.68 2.04 0.24 0.59 251 24.5 0.16 18.2 31.0 7.46 11.1 6.82 1 497 1.1 0.71 2.29 0.22 0.70 254 20.9 0.18 15.3 27.9 6.50 13.6 5.95 1 476 0.9 0.64 1.60 0.20 0.48 273 21.8 0.17 16.0 29.9 6.93 14.3 6.60 1 490 1.0 0.68 1.72 0.21 0.53 276 21.5 0.15 16.3 28.7 6.76 13.8 5.90 1 473 1.0 0.63 1.77 0.18 0.51 256 23.1 0.20 17.4 30.8 7.16 13.8 6.25 1 471 1.1 0.71 1.88 0.25 0.54 265 21.0 0.18 16.4 28.8 6.64 12.0 6.68 1 470 1.0 0.71 1.80 0.20 0.51 281 18.6 0.16 14.6 26.8 6.21 11.4 5.84 1 422 0.9 0.66 1.45 0.20 0.44 283 21.0 0.17 15.6 29.0 6.64 12.3 6.41 1 455 1.0 0.66 1.65 0.21 0.51 276 20.2 0.18 14.9 27.9 6.45 12.4 6.06 1 437 0.9 0.64 1.65 0.21 0.51 261 19.8 0.16 14.6 26.4 6.22 10.9 5.83 1 397 0.9 0.64 1.51 0.17 0.41 256 19.9 0.15 15.2 27.1 6.28 12.1 5.83 1 389 0.9 0.61 1.58 0.18 0.50 241 18.5 0.17 14.1 24.9 6.01 11.2 5.49 1 422 0.9 0.58 1.45 0.19 0.45 219 17.8 0.13 13.3 23.7 5.60 10.8 5.44 1 376 0.8 0.56 1.38 0.17 0.45 220 16.0 0.15 11.8 21.9 5.06 9.6 4.64 1 339 0.7 0.51 1.26 0.17 0.38 195 15.0 0.14 11.2 20.7 4.86 9.2 4.57 1 321 0.7 0.52 1.16 0.16 0.32 177 14.0 0.12 10.7 20.4 4.57 8.9 4.55 1 261 0.6 0.51 1.14 0.15 0.35 184 12.5 0.10 9.2 19.1 4.32 7.6 4.28 1 219 0.6 0.47 0.97 0.15 0.29 182 12.5 0.08 10.1 15.0 3.62 9.1 2.92 1 94.7 0.6 0.31 1.04 0.08 0.31 99 11.5 0.09 9.1 14.4 3.51 7.8 2.93 <1 170.5 0.5 0.32 0.99 0.10 0.31 123 9.4 0.08 7.4 12.7 2.91 5.9 2.45 <1 207 0.4 0.29 0.72 0.08 0.24 142 9.8 0.09 7.5 13.9 3.20 5.7 3.10 <1 194.5 0.5 0.36 0.74 0.08 0.24 104 8.1 0.07 6.0 11.5 2.66 5.1 2.53 <1 187.5 0.4 0.30 0.59 0.09 0.21 101 8.8 0.08 6.7 12.3 2.82 5.3 2.53 1 145.0 0.4 0.31 0.77 0.10 0.28 104 11.2 0.09 9.3 15.4 3.51 7.8 3.43 1 143.5 0.5 0.37 1.05 0.08 0.32 135

<1 11.8 0.88 97 48.3 5.81 12.55 13.40 15.25 1.22 0.46 0.20 1.28 0.19 0.11 <1 11.8 0.84 96 48.0 5.95 13.00 13.25 15.15 1.22 0.48 0.19 1.33 0.19 0.11 <1 11.8 0.98 107 46.7 6.49 12.55 11.60 14.75 1.40 0.42 0.17 1.33 0.17 0.12 <1 13.6 1.12 109 46.6 7.45 12.45 11.55 14.10 1.55 0.39 0.17 1.42 0.17 0.14 <1 11.5 0.89 86 49.4 7.30 13.10 13.25 13.70 1.45 0.48 0.16 1.30 0.19 0.10 <1 11.9 0.89 91 47.4 7.20 12.20 13.20 12.60 1.61 0.38 0.13 1.43 0.18 0.11 <1 14.1 0.93 112 49.4 6.91 12.55 13.35 12.90 1.61 0.34 0.13 1.54 0.18 0.14 <1 14.0 1.18 133 48.4 7.26 12.75 12.85 12.05 1.89 0.41 0.13 1.63 0.18 0.15 1 14.7 1.13 147 48.6 8.51 12.20 12.10 10.95 2.34 0.51 0.13 1.57 0.18 0.18 <1 14.8 1.10 221 48.4 8.27 12.25 11.95 11.00 2.31 0.37 0.13 1.55 0.18 0.18 1 15.1 1.15 163 49.5 8.25 13.35 12.10 11.35 2.32 0.51 0.14 1.72 0.19 0.19 <1 16.4 1.32 180 49.7 8.05 12.50 12.30 11.15 2.37 0.48 0.12 1.71 0.18 0.21 1 15.4 1.31 178 50.0 9.02 12.00 11.75 10.50 2.56 0.43 0.11 1.66 0.17 0.19 <1 14.7 1.20 152 49.1 8.59 12.75 12.20 10.65 2.36 0.57 0.10 1.72 0.18 0.17 <1 15.4 1.21 156 50.0 8.70 12.85 12.45 10.90 2.34 0.55 0.11 1.72 0.18 0.18 <1 14.6 1.14 151 48.3 8.48 12.35 11.50 10.45 2.25 0.53 0.10 1.63 0.17 0.17 <1 16.1 1.28 165 49.7 8.69 12.90 12.15 10.55 2.41 0.54 0.11 1.80 0.19 0.21 1 15.9 1.38 158 49.4 9.38 12.35 11.65 11.30 2.43 0.49 0.10 1.73 0.17 0.18 <1 14.4 1.28 132 49.1 8.64 13.05 12.45 11.05 2.25 0.47 0.10 1.71 0.19 0.17 <1 15.4 1.24 156 49.2 7.97 12.70 12.10 11.20 2.10 0.50 0.11 1.63 0.18 0.16 <1 14.8 1.09 152 48.8 7.93 12.85 12.50 11.40 2.16 0.49 0.12 1.63 0.19 0.17 <1 14.7 1.20 141 48.1 7.58 12.75 12.55 11.80 2.05 0.43 0.13 1.56 0.18 0.15 1 14.2 1.18 145 48.0 7.32 12.95 11.80 12.75 1.94 0.46 0.15 1.54 0.18 0.16 <1 13.4 1.07 131 48.6 7.31 13.25 12.05 13.20 1.98 0.46 0.17 1.46 0.19 0.15 <1 12.7 1.13 124 49.5 7.10 13.30 12.55 14.15 1.84 0.44 0.18 1.42 0.19 0.14 <1 12.0 0.90 112 48.5 6.40 13.30 12.25 14.90 1.72 0.43 0.20 1.38 0.19 0.13 <1 11.2 0.90 107 48.7 6.13 13.10 12.35 15.85 1.61 0.43 0.22 1.31 0.19 0.13 <1 11.3 0.91 102 48.3 5.70 12.40 12.95 16.15 1.35 0.37 0.23 1.25 0.19 0.11 <1 10.6 0.82 92 48.2 5.27 11.85 13.75 16.70 1.13 0.30 0.26 1.16 0.19 0.10 <1 7.2 0.57 92 41.4 3.93 16.90 5.97 22.0 0.47 0.26 0.22 0.94 0.25 0.11 <1 7.3 0.56 83 41.9 3.96 17.15 6.06 23.2 0.85 0.33 0.30 0.99 0.22 0.10 <1 6.4 0.53 66 40.6 4.22 17.70 5.74 23.4 0.85 0.27 0.41 1.02 0.22 0.08 <1 7.3 0.61 69 43.3 4.20 15.85 7.60 22.1 0.87 0.25 0.34 0.88 0.21 0.08 <1 6.3 0.50 59 43.1 3.94 15.50 8.28 22.2 0.77 0.22 0.33 0.83 0.21 0.07 <1 7.1 0.61 69 43.1 3.76 15.30 7.90 22.2 0.64 0.17 0.34 0.81 0.20 0.09 <1 8.0 0.65 85 42.4 3.93 15.90 7.87 21.7 0.68 0.27 0.32 0.96 0.21 0.10

0.04 0.02 1.55 100.38 <0.5 <5 <0.5 77 176 20 <1 345 7 39 <10 0.04 0.02 1.55 100.48 <0.5 <5 <0.5 77 157 20 <1 324 5 37 <10 0.04 0.01 1.64 97.39 <0.5 <5 <0.5 77 122 10 <1 346 4 33 <10 0.04 0.01 3.10 99.14 <0.5 <5 <0.5 66 134 20 <1 293 7 33 10 0.05 0.01 1.45 101.94 <0.5 <5 <0.5 70 103 10 <1 262 3 37 <10 0.04 0.01 1.92 98.41 <0.5 <5 <0.5 64 79 10 <1 210 6 40 <10 0.04 0.01 1.61 100.71 <0.5 <5 <0.5 63 127 20 <1 209 5 41 <10 0.05 0.02 1.19 98.96 <0.5 <5 0.5 66 180 10 <1 209 7 41 <10 0.05 0.02 1.47 98.81 <0.5 <5 <0.5 60 151 10 <1 204 <2 33 <10 0.6 19 <0.5 122 1225 20 <1 1890 5 14 <10 0.05 0.02 1.34 98.00 <0.5 <5 <0.5 64 463 10 <1 228 5 35 <10 0.06 0.02 1.12 100.82 <0.5 <5 <0.5 65 194 10 <1 209 4 34 <10 0.05 0.02 0.98 99.82 <0.5 <5 <0.5 62 203 10 <1 204 6 36 <10 0.06 0.02 1.27 99.74 <0.5 <5 0.5 61 849 20 <1 270 10 33 <10 0.06 0.02 0.76 99.23 <0.5 <5 <0.5 61 110 10 <1 172 4 35 <10 0.06 0.02 0.93 100.99 <0.5 <5 <0.5 59 147 10 <1 178 3 34 10 0.06 0.02 0.97 96.98 <0.5 <5 <0.5 63 311 10 <1 199 3 34 <10 <0.5 <5 <0.5 25 25 10 <1 22 6 11 <10 0.05 0.02 0.82 100.14 <0.5 <5 <0.5 64 109 10 <1 187 6 36 <10 0.06 0.02 1.61 100.87 <0.5 <5 <0.5 60 126 20 <1 180 3 37 <10 0.05 0.02 1.51 100.76 <0.5 <5 <0.5 64 108 10 <1 183 3 37 <10 0.05 0.02 0.65 98.57 <0.5 <5 <0.5 67 116 10 <1 196 6 39 10 0.05 0.02 0.81 99.12 <0.5 <5 <0.5 65 105 10 <1 202 2 38 <10 0.05 0.02 0.85 98.20 <0.5 <5 <0.5 67 99 10 <1 217 3 37 <10 0.04 0.02 1.03 98.34 <0.5 <5 <0.5 71 100 10 <1 254 4 36 <10 0.05 0.02 0.42 99.31 <0.5 <5 <0.5 69 89 10 <1 265 3 33 <10 0.04 0.02 1.11 101.98 <0.5 <5 <0.5 71 94 10 <1 290 4 34 <10 0.04 0.02 0.50 99.96 <0.5 <5 <0.5 75 98 10 <1 329 5 34 <10 0.04 0.02 0.61 100.69 <0.5 <5 <0.5 77 132 10 <1 361 3 34 <10 0.5 16 <0.5 124 1270 20 <1 1960 9 14 10 0.03 0.01 1.21 100.25 <0.5 <5 <0.5 75 135 10 <1 365 <2 35 10 0.03 0.01 1.94 100.89 <0.5 <5 <0.5 71 260 10 <1 358 6 38 <10 0.01 <0.01 8.50 100.96 <0.5 <5 <0.5 138 140 20 <1 772 6 18 <10 0.02 0.01 6.55 101.64 <0.5 <5 <0.5 127 147 10 <1 716 <2 18 10 0.02 0.01 6.02 100.56 <0.5 <5 <0.5 131 272 10 <1 763 6 17 <10 0.02 0.01 5.09 100.80 <0.5 <5 <0.5 121 328 10 <1 699 2 23 <10 0.02 0.01 5.01 100.49 <0.5 <5 <0.5 128 398 10 <1 757 2 26 <10 0.01 0.01 5.77 100.30 1.2 6 1.0 134 2090 20 <1 1160 5 25 <10 0.02 0.01 5.33 99.70 2.2 <5 <0.5 140 3040 20 <1 1510 14 25 <10 1.9 <5 0.6 146 2840 20 <1 1570 11 26 <10

87 0.08 3.17 84 0.06 82 0.51 82 0.35 92 0.06 80 0.24 3.16 78 0.30 97 0.14 88 0.09 99 109 0.43 101 0.23 112 0.13 144 0.52 3.07 91 0.07 97 0.12 94 0.23 61 112 0.11 122 0.16 150 0.10 3.12 98 0.04 96 0.07 91 0.04 91 0.06 88 0.02 87 0.02 88 0.02 86 0.02 102 82 0.03 74 0.04 98 0.08 101 0.02 107 0.06 2.99 96 0.23 95 0.12 515 0.93 135 0.86 135

2.59 0.023 0.166 0.100 53.7 18.6 2550 1.57 1.43 0.70 0.74 5.5 2.08 1.8 0.27 2.60 0.017 0.157 0.109 103.0 26.7 2080 2.11 1.71 0.91 0.87 7.2 2.73 2.3 0.33 2.51 0.007 0.237 0.129 33.6 15.4 2770 1.42 1.25 0.63 0.60 4.6 1.91 1.3 0.22 2.44 0.057 0.550 0.426 18.1 8.7 2880 1.46 0.96 0.37 0.43 3.6 1.33 0.9 0.19 2.51 0.032 0.249 0.206 30.7 13.7 2240 1.77 1.22 0.57 0.56 5.3 2.05 1.2 0.22 2.49 0.025 0.303 0.213 38.2 13.6 2640 2.23 1.32 0.59 0.70 5.8 1.90 1.3 0.25 2.43 0.021 0.187 0.070 34.7 11.4 2770 1.14 1.26 0.52 0.52 3.9 1.77 1.1 0.21 1.89 0.021 0.052 0.029 26.6 16.0 2400 2.45 1.40 0.59 0.61 5.4 1.94 1.5 0.25 2.43 0.017 0.080 0.050 22.8 11.6 2480 1.68 1.37 0.56 0.67 4.8 1.67 1.1 0.21 0.07 0.166 1.800 0.824 2.62 0.009 0.075 0.051 15.1 8.8 2440 0.81 1.13 0.55 0.55 4.1 1.93 0.9 0.21 2.82 0.034 0.685 0.266 21.1 9.9 2830 0.82 1.21 0.56 0.56 4.0 1.67 1.0 0.22 2.73 0.030 0.233 0.137 22.6 8.3 2670 0.92 1.13 0.44 0.52 3.7 1.68 0.7 0.20 2.73 0.045 0.779 0.518 19.7 11.7 2390 1.26 1.39 0.62 0.61 4.7 1.90 1.1 0.25 2.56 0.075 1.065 0.670 38.6 17.4 2340 1.37 1.83 0.73 0.85 6.0 2.57 1.4 0.30 2.64 0.074 0.722 0.393 31.4 19.5 2210 1.17 1.98 0.82 0.90 6.3 2.74 1.6 0.36 2.65 0.057 0.658 0.428 45.4 22.7 1880 1.09 2.14 1.06 0.97 6.6 3.01 2.0 0.37 2.70 0.093 1.290 0.703 29.4 19.7 1970 1.38 2.10 0.92 0.98 6.4 2.82 1.7 0.34 2.69 0.059 0.830 0.466 33.5 21.7 1820 1.65 2.41 1.08 1.08 7.1 3.32 2.0 0.41 2.89 0.101 1.510 0.918 42.0 18.0 2060 1.52 2.28 0.96 1.02 6.8 2.99 1.7 0.38 2.91 0.092 1.970 1.515 50.2 17.5 2010 1.47 2.39 1.08 0.95 7.0 3.29 1.9 0.42 1.16 0.165 2.29 1.305 1.62 0.140 2.33 1.280 124.0 29.6 1280 3.92 3.11 1.45 1.29 10.5 4.41 2.8 0.54 0.70 <0.001 0.011 0.008 2.68 0.138 2.12 1.210 177.0 43.2 1490 3.88 3.42 1.63 1.52 12.7 4.74 3.8 0.58 2.38 0.146 1.925 1.010 158.0 33.9 1820 3.61 2.84 1.42 1.39 11.1 4.06 2.9 0.57 2.74 0.016 0.116 0.071 512 66.0 270 3.29 2.74 1.39 1.30 18.7 3.66 4.2 0.49 2.38 0.001 0.047 0.026 466 61.8 950 1.77 2.77 1.39 1.11 17.3 3.84 3.9 0.47 1.07 0.002 0.024 0.010 472 66.6 220 2.41 2.55 1.42 1.34 17.9 3.74 3.9 0.48 0.06 0.168 1.840 0.833 1.14 0.068 1.195 0.909 299 62.1 180 1.70 2.78 1.46 1.11 19.4 3.64 3.7 0.49 2.29 0.029 0.223 0.130 2.28 0.001 <0.005 0.002 2.31 <0.001 <0.005 0.002 2.21 <0.001 <0.005 0.001 2.45 <0.001 <0.005 0.001 2.34 <0.001 <0.005 0.001 342 69.9 220 0.97 2.92 1.69 1.25 21.5 3.99 4.6 0.55 2.30 <0.001 <0.005 0.002 2.33 <0.001 <0.005 0.001 <0.02 <0.001 <0.005 0.001

7.9 0.08 6.2 11.2 2.57 6.4 2.60 1 133.0 0.3 0.30 0.63 0.09 0.21 119 11.4 0.11 8.7 15.5 3.67 10.6 3.27 1 180.5 0.5 0.36 0.95 0.11 0.26 163 6.4 0.05 4.4 9.9 2.17 4.6 2.19 <1 96.6 0.2 0.27 0.45 0.07 0.12 113 3.3 0.04 2.5 6.3 1.28 2.8 1.54 <1 75.6 0.1 0.20 0.20 0.05 0.06 98 5.5 0.05 4.1 8.9 1.94 4.0 2.09 1 121.0 0.2 0.26 0.32 0.08 0.10 124 5.4 0.05 4.5 9.1 1.96 4.3 2.15 1 131.5 0.2 0.26 0.38 0.08 0.09 171 4.3 0.07 3.2 8.0 1.68 4.1 1.87 <1 107.0 0.1 0.25 0.33 0.06 0.10 114 7.1 0.08 4.0 9.9 2.11 5.5 1.99 <1 84.8 0.2 0.23 1.22 0.06 0.39 111 5.0 0.06 3.3 8.3 1.75 3.7 2.13 <1 66.9 0.2 0.24 0.61 0.06 0.21 116 3.1 0.06 2.1 7.3 1.41 1.8 1.65 <1 81.1 0.1 0.24 0.16 0.06 0.06 128 3.8 0.06 2.4 7.3 1.54 2.3 1.78 <1 74.2 0.1 0.25 0.33 0.05 0.07 118 2.9 0.04 1.9 6.6 1.29 2.6 1.64 <1 64.3 0.1 0.21 0.15 0.06 0.15 122 4.7 0.06 3.1 8.6 1.82 3.2 1.91 <1 80.3 0.1 0.26 0.33 0.06 0.09 155 6.8 0.07 5.2 12.0 2.45 4.6 2.88 1 113.5 0.2 0.34 0.50 0.10 0.17 180 7.5 0.08 7.6 13.8 2.84 3.8 2.96 1 102.0 0.3 0.37 0.54 0.10 0.15 163 8.9 0.10 7.3 14.6 3.21 3.9 3.43 1 106.5 0.4 0.40 0.73 0.12 0.20 170 7.6 0.10 5.6 13.7 2.85 4.8 3.20 1 89.4 0.3 0.39 0.52 0.11 0.17 174 8.5 0.09 6.1 14.9 3.11 6.1 3.56 1 87.2 0.3 0.39 0.73 0.13 0.23 190 6.9 0.10 5.1 13.5 2.68 6.0 3.35 1 118.0 0.2 0.43 0.42 0.12 0.14 197 6.6 0.11 4.2 13.6 2.80 6.9 3.50 1 95.9 0.2 0.47 0.76 0.12 0.22 202 11.8 0.13 7.9 20.5 4.30 19.0 4.83 1 222 0.5 0.57 1.53 0.16 0.49 287 18.2 0.16 12.1 26.2 5.82 20.7 5.59 1 339 0.7 0.66 2.24 0.17 0.60 252 13.9 0.15 9.0 21.8 4.85 19.5 4.60 1 259 0.5 0.58 2.24 0.17 0.66 210 32.9 0.19 6.3 29.2 7.56 38.5 4.61 1 540 0.4 0.48 8.00 0.21 2.39 128 29.8 0.20 6.9 27.5 7.20 32.3 4.86 1 470 0.4 0.47 8.44 0.20 2.37 113 34.9 0.20 6.6 28.9 7.58 36.8 5.19 1 447 0.4 0.51 8.37 0.20 2.19 109 29.9 0.19 9.0 28.7 7.49 27.1 4.86 1 339 0.9 0.51 8.22 0.19 1.99 113 34.4 0.23 8.2 30.9 8.19 29.6 5.30 1 412 0.5 0.49 10.30 0.22 2.50 134

<1 6.4 0.52 66 42.1 3.18 14.15 7.81 23.7 0.50 0.21 0.35 0.77 0.20 0.06 <1 8.1 0.67 80 42.1 4.23 15.15 7.51 22.2 0.66 0.35 0.29 1.00 0.20 0.10 <1 5.9 0.44 39 42.9 2.49 13.70 9.30 23.8 0.40 0.15 0.38 0.65 0.20 0.05 <1 4.3 0.39 26 42.5 1.90 13.80 9.22 25.0 0.29 0.07 0.40 0.52 0.19 0.03 <1 5.5 0.44 36 42.9 2.84 14.30 9.71 23.2 0.44 0.12 0.31 0.74 0.20 0.04 <1 5.5 0.47 38 41.7 3.00 15.85 8.41 23.0 0.44 0.13 0.36 0.94 0.20 0.05 <1 5.3 0.55 35 44.1 2.37 13.55 10.90 23.1 0.36 0.12 0.39 0.64 0.19 0.04 <1 6.1 0.49 51 45.8 3.31 12.25 10.25 21.8 0.75 0.14 0.33 0.58 0.22 0.04 <1 5.6 0.44 33 43.5 2.58 12.45 10.70 22.3 0.34 0.10 0.34 0.59 0.23 0.03 <1 5.2 0.44 21 43.8 2.01 12.75 12.05 22.2 0.31 0.06 0.33 0.60 0.18 0.02 <1 5.0 0.41 25 43.6 2.03 13.65 11.10 23.0 0.33 0.08 0.39 0.57 0.19 0.03 <1 4.9 0.42 17 44.7 1.83 13.30 12.25 22.7 0.26 0.07 0.37 0.57 0.18 0.02 <1 5.8 0.40 31 43.3 2.50 15.30 11.00 22.1 0.34 0.09 0.33 0.73 0.20 0.03 <1 7.3 0.56 49 44.0 3.35 14.85 11.95 19.75 0.49 0.14 0.32 0.95 0.19 0.05 <1 8.4 0.67 47 46.1 3.46 12.25 13.90 19.00 0.51 0.13 0.31 0.97 0.18 0.06 <1 8.9 0.67 63 46.8 4.15 11.70 13.90 18.05 0.75 0.12 0.26 1.05 0.18 0.07 <1 9.1 0.77 51 46.2 3.65 12.85 13.50 18.10 0.53 0.14 0.27 0.96 0.19 0.06 <1 9.7 0.78 63 46.8 4.11 13.20 13.80 17.80 0.60 0.17 0.25 1.07 0.21 0.07 1 9.2 0.73 52 46.2 3.70 14.60 13.45 18.35 0.58 0.18 0.29 1.06 0.19 0.06 <1 9.9 0.73 58 46.1 3.84 14.55 13.70 17.40 0.59 0.18 0.27 1.09 0.18 0.06 1 13.0 1.02 93 45.2 6.16 16.60 10.90 14.55 1.01 0.45 0.17 1.69 0.20 0.13 1 14.5 1.16 134 45.0 7.64 15.85 10.15 13.15 1.39 0.53 0.20 1.82 0.18 0.15 <1 13.0 1.09 87 47.9 6.50 14.55 9.53 15.15 1.19 0.55 0.25 1.54 0.19 0.12 2 13.4 1.34 159 62.0 14.95 7.43 3.96 4.25 3.83 1.34 0.04 0.65 0.13 0.17 1 13.2 1.38 142 64.1 14.85 6.19 4.01 3.42 4.33 1.23 0.13 0.58 0.12 0.17 1 13.5 1.35 149 62.5 15.00 6.36 4.12 3.49 4.42 1.28 0.03 0.60 0.12 0.16 1 13.4 1.19 140 59.5 14.55 7.93 5.26 3.64 4.85 1.01 0.02 0.56 0.13 0.17 1 14.9 1.62 170 58.8 15.80 7.10 3.45 4.16 5.40 1.10 0.03 0.68 0.12 0.19

0.01 0.01 6.37 99.42 <0.5 <5 <0.5 127 637 10 <1 846 3 26 <10 0.02 0.01 5.45 99.27 0.7 <5 <0.5 134 982 20 <1 914 8 25 <10 0.01 <0.01 5.95 99.98 <0.5 <5 <0.5 124 423 10 <1 726 6 30 10 0.01 <0.01 6.32 100.25 0.9 <5 <0.5 123 1130 10 <1 888 7 30 <10 0.01 <0.01 5.82 100.63 1.2 <5 1.2 123 812 20 <1 775 9 30 10 0.02 <0.01 5.88 99.98 <0.5 5 <0.5 137 583 10 <1 815 8 29 <10 0.01 <0.01 4.53 100.30 <0.5 <5 0.9 113 289 <10 <1 686 4 32 <10 0.01 <0.01 5.32 100.80 <0.5 <5 0.7 102 314 10 <1 619 2 30 <10 0.01 <0.01 6.26 99.43 0.5 <5 0.9 102 461 10 <1 638 <2 32 <10 <0.5 <5 <0.5 97 820 <10 <1 1820 12 23 <10 0.01 <0.01 4.73 99.05 <0.5 <5 0.9 110 520 <10 <1 649 2 37 <10 0.01 <0.01 4.81 99.79 <0.5 <5 0.9 123 802 <10 <1 777 3 33 <10 0.01 <0.01 4.16 100.42 0.5 <5 0.7 114 870 <10 <1 758 <2 36 <10 0.01 <0.01 3.89 99.82 1.1 <5 0.9 137 2100 <10 <1 1150 5 33 <10 0.01 <0.01 3.41 99.46 1.5 <5 1.0 128 2540 10 <1 1130 3 36 <10 0.01 <0.01 2.19 99.07 1.3 <5 1.0 94 1725 10 <1 779 <2 39 10 0.01 0.01 2.29 99.34 1.4 <5 1.3 85 1820 10 <1 717 5 39 10 0.01 <0.01 2.59 99.05 1.3 <5 1.1 109 2610 20 1 983 4 41 <10 0.01 <0.01 2.39 100.48 1.2 <5 1.6 98 1605 20 <1 722 3 41 10 0.01 <0.01 1.70 100.37 1.7 <5 0.7 112 2800 10 <1 1060 4 39 <10 0.01 0.01 2.09 100.07 1.8 <5 1.1 131 4000 20 <1 1750 2 39 10 4.0 <5 1.4 121 5700 30 <1 1890 8 37 <10 0.03 0.01 2.17 99.27 2.6 <5 1.4 131 4360 20 <1 1580 7 35 10 <0.5 <5 <0.5 28 60 20 <1 37 9 13 <10 0.04 0.02 1.95 98.07 2.5 5 0.5 131 4710 30 <1 1880 10 31 <10 0.03 0.02 1.64 99.16 2.5 <5 0.7 118 3920 30 <1 1570 14 31 <10 0.06 0.06 2.93 101.80 <0.5 <5 <0.5 30 385 60 <1 144 16 16 <10 0.05 0.05 2.71 101.94 <0.5 <5 <0.5 19 254 50 <1 119 24 14 <10 0.05 0.05 2.71 100.89 <0.5 <5 <0.5 25 166 50 <1 84 14 14 <10 <0.5 7 <0.5 99 873 10 <1 1930 15 24 <10 0.04 0.03 2.92 100.61 2.2 <5 0.8 65 2290 50 <1 1440 95 13 10 <0.5 <5 <0.5 18 601 60 <1 125 35 14 <10 <0.5 <5 <0.5 26 101 50 <1 84 6 13 <10 <0.5 <5 <0.5 21 53 40 <1 72 7 13 <10 <0.5 <5 <0.5 18 66 40 1 61 4 12 <10 <0.5 <5 <0.5 20 42 40 <1 64 7 13 <10 0.05 0.04 3.34 100.26 <0.5 <5 <0.5 25 83 50 <1 86 3 14 <10 <0.5 <5 <0.5 12 52 30 <1 71 8 14 <10 <0.5 <5 <0.5 19 66 40 <1 69 14 13 <10 <0.5 <5 <0.5 20 65 40 <1 69 9 13 <10

104 0.40 2.95 98 0.31 109 0.45 104 0.57 431 1.23 93 0.28 3.02 126 0.53 168 0.22 142 0.42 82 77 0.44 74 0.35 70 0.28 79 0.66 3.13 92 0.97 112 0.77 112 0.88 126 1.21 216 0.87 72 0.87 70 1.47 3.25 110 106 1.13 66 113 1.29 111 1.04 67 0.26 64 0.17 2.75 35 0.18 89 487 0.89 196 47 47 46 59 53 0.24 2.70 338 44 44

2.20 0.001 <0.005 0.002 2.38 <0.001 <0.005 0.001 2.35 <0.001 <0.005 0.002 445 77.3 180 2.35 2.93 1.47 1.31 18.5 3.81 4.6 0.56 2.50 <0.001 <0.005 0.001 2.31 0.001 <0.005 0.001 2.35 <0.001 <0.005 0.002 2.50 <0.001 <0.005 0.001 2.34 <0.001 <0.005 0.001 810 84.7 170 4.48 2.94 1.61 1.42 19.2 4.46 4.9 0.59 2.43 <0.001 <0.005 0.002 0.07 0.039 0.183 0.354 2.36 <0.001 <0.005 0.002 2.42 <0.001 <0.005 0.003 2.36 0.001 <0.005 0.002 2.27 <0.001 <0.005 0.001 505 59.3 180 4.70 2.76 1.65 1.10 20.3 3.84 3.8 0.54 2.29 0.003 <0.005 0.020 2.39 <0.001 <0.005 0.002 2.52 <0.001 <0.005 0.002 1.01 <0.001 <0.005 <0.001

39.6 0.21 8.1 31.5 8.72 60.3 5.40 1 539 0.5 0.49 10.95 0.20 2.79 108 44.0 0.22 9.5 34.6 9.35 100.0 5.70 1 551 0.5 0.51 12.35 0.21 3.52 115 29.4 0.24 6.7 25.9 6.72 73.7 4.56 1 523 0.4 0.48 7.17 0.24 1.99 132

1 14.5 1.59 182 64.7 14.80 6.49 3.88 3.04 3.88 1.72 0.02 0.57 0.07 0.16 1 15.1 1.51 190 64.1 15.80 6.64 3.21 3.09 3.08 3.06 0.02 0.62 0.08 0.16 1 14.7 1.59 132 63.5 16.20 6.99 2.21 3.01 4.82 2.28 0.02 0.63 0.09 0.17

<0.5 <5 <0.5 18 83 30 <1 71 8 12 <10 <0.5 <5 <0.5 20 66 30 <1 64 12 12 <10 0.06 0.05 2.42 101.86 <0.5 <5 <0.5 19 61 30 <1 65 13 12 <10 <0.5 <5 <0.5 19 56 30 <1 65 20 13 <10 <0.5 <5 <0.5 20 61 40 <1 68 17 13 <10 <0.5 <5 <0.5 22 55 40 <1 67 22 13 <10 <0.5 <5 <0.5 19 53 40 1 62 14 12 <10 0.06 0.09 1.81 101.82 <0.5 <5 <0.5 22 60 40 <1 69 17 13 <10 <0.5 <5 <0.5 25 47 40 1 81 15 15 <10 <0.5 10 0.6 126 1250 20 1 1980 3 14 <10 <0.5 <5 <0.5 22 63 40 <1 71 15 14 <10 <0.5 <5 <0.5 24 53 40 1 68 10 13 <10 <0.5 <5 <0.5 24 120 50 <1 72 13 15 <10 0.06 0.06 1.60 101.64 <0.5 <5 <0.5 26 47 40 <1 82 12 17 <10 <0.5 <5 <0.5 18 92 30 <1 56 22 12 <10 <0.5 <5 <0.5 29 66 40 2 94 13 19 <10 <0.5 <5 <0.5 22 72 30 1 76 15 14 <10 <0.5 <5 <0.5 29 52 10 <1 27 12 10 <10

48 49 51 0.27 2.76 59 61 64 68 63 0.28 2.79 42 102 69 75 79 49 0.27 2.74 123 49 65 79

2.19 0.001 <0.005 0.003 91 57 29 <0.5 2.06 <0.001 <0.005 0.003 95 62 26 <0.5 2.13 <0.001 <0.005 0.003 85 185 23 <0.5 2.05 0.001 <0.005 0.003 84 81 26 <0.5 1.99 0.001 <0.005 0.002 93 60 24 <0.5 2.19 <0.001 <0.005 0.002 86 13 25 <0.5 2.15 <0.001 <0.005 0.002 78 24 23 <0.5 2.06 <0.001 <0.005 0.003 66 29 22 <0.5 1.97 <0.001 0.005 0.005 47 50 22 <0.5 2.11 <0.001 <0.005 <0.001 <1 12 15 <0.5 2.14 <0.001 <0.005 0.001 <1 5 17 <0.5 0.07 0.034 0.178 0.347 1965 1310 129 <0.5 2.17 <0.001 <0.005 0.001 2 8 19 <0.5 2.25 <0.001 <0.005 <0.001 <1 4 17 <0.5 2.25 <0.001 <0.005 <0.001 <1 7 23 <0.5 2.12 <0.001 <0.005 <0.001 <1 2 20 <0.5 3.44 0.001 <0.005 <0.001 <1 73 29 <0.5 3.49 <0.001 <0.005 <0.001 <1 47 38 <0.5 3.40 <0.001 <0.005 <0.001 <1 2 35 <0.5 3.38 <0.001 <0.005 0.001 1 48 34 <0.5 3.52 <0.001 <0.005 0.001 19 192 41 <0.5 0.81 <0.001 <0.005 0.001 23 29 26 <0.5 3.57 <0.001 <0.005 0.001 2 69 32 <0.5 3.45 <0.001 <0.005 <0.001 <1 20 28 <0.5 3.30 <0.001 <0.005 0.001 <1 19 22 <0.5 3.27 <0.001 <0.005 <0.001 <1 15 15 <0.5 3.28 <0.001 <0.005 <0.001 <1 14 14 <0.5 3.29 <0.001 <0.005 0.001 <1 25 12 <0.5 3.36 <0.001 <0.005 <0.001 <1 14 13 <0.5 3.15 <0.001 <0.005 <0.001 <1 10 10 <0.5 3.17 <0.001 <0.005 0.001 <1 9 10 <0.5 0.06 0.035 0.173 0.339 2100 1400 138 0.7 2.88 <0.001 <0.005 0.001 3 8 12 <0.5 2.70 <0.001 <0.005 0.001 <1 1 26 <0.5 3.24 <0.001 <0.005 <0.001 <1 9 21 <0.5 3.11 <0.001 <0.005 0.001 <1 14 32 <0.5 3.47 <0.001 <0.005 0.001 <1 18 38 <0.5 2.37 <0.001 <0.005 0.001 <1 24 51 <0.5 2.26 <0.001 <0.005 <0.001 3 16 27 <0.5 2.11 <0.001 <0.005 <0.001 5 21 36 <0.5

2.29 <0.001 <0.005 <0.001 1 32 48 <0.5 <0.02 <0.001 <0.005 <0.001 3 30 51 <0.5 2.33 <0.001 <0.005 <0.001 3 16 46 <0.5 2.21 <0.001 <0.005 <0.001 3 25 41 <0.5 2.02 <0.001 <0.005 <0.001 1 23 45 <0.5 2.36 <0.001 <0.005 <0.001 1 27 49 <0.5 2.27 <0.001 <0.005 <0.001 1 23 37 <0.5 2.31 <0.001 <0.005 <0.001 2 21 38 <0.5 2.32 <0.001 <0.005 <0.001 1 19 37 <0.5 2.37 <0.001 <0.005 <0.001 1 22 49 <0.5 3.43 <0.001 <0.005 <0.001 1 32 40 <0.5 0.06 0.031 0.170 0.329 1895 1260 122 <0.5 3.51 <0.001 <0.005 <0.001 5 53 51 <0.5 3.59 <0.001 <0.005 <0.001 9 68 54 <0.5 3.50 <0.001 <0.005 <0.001 15 238 59 <0.5 3.44 <0.001 <0.005 <0.001 37 423 63 <0.5 3.64 <0.001 <0.005 <0.001 65 524 67 <0.5 3.72 <0.001 <0.005 <0.001 122 698 82 <0.5 3.67 0.003 <0.005 <0.001 145 770 67 <0.5 3.38 0.004 <0.005 <0.001 89 263 41 <0.5 3.40 0.016 <0.005 <0.001 116 308 47 <0.5 0.99 0.001 <0.005 <0.001 27 27 25 <0.5 2.34 0.025 0.145 0.012 124 287 43 <0.5 2.34 0.038 0.168 0.017 124 300 42 <0.5 2.40 0.046 0.320 0.045 118 351 41 <0.5 2.31 0.032 0.191 0.024 128 307 42 <0.5 2.25 0.019 0.200 0.032 144 283 46 <0.5 2.59 0.029 0.337 0.140 190 202 57 <0.5 2.30 0.034 0.387 0.272 213 191 67 <0.5 2.44 0.004 0.338 0.246 256 141 71 <0.5 2.60 0.001 0.288 0.168 235 122 67 <0.5 0.07 0.031 0.169 0.329 1920 1285 123 0.5 2.54 0.002 0.256 0.144 208 82 60 <0.5 2.46 0.001 0.157 0.122 169 70 54 <0.5 2.50 0.002 0.089 0.095 167 54 56 <0.5 2.49 0.001 0.096 0.099 181 76 58 <0.5 2.59 0.001 0.144 0.100 194 80 62 <0.5 2.41 0.001 0.053 0.069 195 79 59 <0.5 2.33 0.001 0.032 0.021 198 86 60 <0.5 2.38 0.001 0.021 0.015 225 83 65 <0.5

2.47 <0.001 0.013 0.011 195 56 61 <0.5 <0.02 0.001 0.014 0.012 194 57 61 <0.5 2.24 0.002 0.028 0.028 182 83 59 <0.5 2.41 0.001 0.015 0.015 216 90 64 <0.5 2.39 0.001 0.013 0.011 233 86 67 <0.5 2.44 <0.001 0.013 0.009 246 92 68 <0.5 3.63 <0.001 0.009 0.004 271 104 73 <0.5 4.01 0.001 0.029 0.012 259 103 71 <0.5 3.86 0.002 0.015 0.008 309 112 77 <0.5 3.78 <0.001 0.012 0.005 341 89 82 <0.5 4.10 0.002 0.019 0.008 348 72 82 <0.5 0.07 0.036 0.182 0.344 2030 1340 133 <0.5 3.59 <0.001 0.011 0.004 346 82 84 <0.5 3.99 0.001 0.008 0.003 364 72 86 <0.5 3.96 0.001 0.012 0.004 396 71 91 <0.5 3.77 <0.001 0.008 0.004 401 62 89 <0.5 3.70 <0.001 0.016 0.004 409 52 91 <0.5 3.71 0.001 0.020 0.008 422 64 92 <0.5 3.43 <0.001 0.006 0.005 414 60 92 <0.5 3.68 <0.001 0.008 0.002 401 53 90 <0.5 3.79 0.001 0.017 0.007 383 52 86 <0.5 0.61 <0.001 <0.005 <0.001 27 26 28 <0.5 3.77 0.001 0.013 0.004 382 58 88 <0.5 3.84 <0.001 0.012 0.003 393 51 86 <0.5 3.81 0.001 0.012 0.003 355 69 78 <0.5 3.27 <0.001 0.016 0.005 397 64 84 <0.5 3.39 <0.001 0.015 0.011 401 65 83 <0.5 3.65 <0.001 0.011 0.005 455 69 89 <0.5 3.59 0.002 0.022 0.010 625 94 115 <0.5 3.71 <0.001 0.017 0.008 604 83 107 <0.5 3.62 0.001 0.025 0.011 736 88 124 <0.5 0.06 0.036 0.171 0.334 1980 1300 127 <0.5 3.72 <0.001 0.030 0.010 783 87 132 <0.5 3.63 0.001 0.030 0.016 758 82 129 <0.5 3.61 0.002 0.018 0.010 680 82 114 <0.5 3.77 0.003 0.038 0.028 757 96 128 <0.5 3.69 <0.001 0.028 0.010 756 81 125 <0.5 3.56 0.001 0.027 0.018 738 90 123 <0.5 3.63 <0.001 0.023 0.007 813 86 136 <0.5 3.50 0.002 0.042 0.044 835 91 137 <0.5

3.52 <0.001 0.023 0.010 785 87 130 <0.5 <0.02 <0.001 0.023 0.011 790 88 131 <0.5 3.59 0.001 0.037 0.022 796 92 131 <0.5 3.31 <0.001 0.032 0.018 809 90 132 <0.5 4.31 0.001 0.039 0.026 794 100 131 <0.5 2.84 <0.001 0.030 0.012 744 97 123 <0.5 3.66 0.001 0.038 0.031 766 113 130 <0.5 3.76 <0.001 0.028 0.016 710 99 122 <0.5 3.74 <0.001 0.033 0.016 614 96 109 <0.5 3.44 <0.001 0.031 0.017 594 126 104 <0.5 3.89 0.005 0.058 0.042 602 251 101 <0.5 0.07 0.032 0.171 0.340 1900 1220 122 <0.5 3.77 0.003 0.042 0.036 550 174 103 <0.5 3.85 0.003 0.033 0.019 497 123 96 <0.5 3.47 0.001 0.018 0.008 427 89 88 <0.5 2.51 0.001 0.022 0.012 449 110 91 <0.5 2.36 <0.001 0.019 0.013 449 104 92 <0.5 2.49 0.002 0.021 0.013 434 137 91 <0.5 2.59 0.007 0.058 0.058 393 312 80 <0.5

2.13 <0.001 <0.005 0.002 <0.5 25 52 87 2.02 <0.001 <0.005 0.003 <0.5 31 26 91 1.85 0.008 <0.005 0.001 <0.5 23 54 85 2.49 0.001 <0.005 0.002 <0.5 26 56 95 2.09 0.001 0.010 0.007 <0.5 23 67 49 2.37 0.001 0.013 0.010 <0.5 23 74 47 1.97 0.012 <0.005 0.003 <0.5 5 56 7 1.40 <0.001 <0.005 0.002 <0.5 3 11 5 0.89 <0.001 0.009 0.007 <0.5 13 11 18 1.62 <0.001 0.007 0.004 <0.5 6 15 11 2.38 <0.001 0.011 0.007 <0.5 17 54 28 2.37 0.001 <0.005 0.003 <0.5 11 25 15 0.06 0.034 0.186 0.362 <0.5 128 1290 1970 1.98 <0.001 <0.005 0.002 <0.5 9 21 14 2.62 <0.001 <0.005 <0.001 <0.5 2 6 2 1.78 <0.001 0.005 0.003 <0.5 17 67 29 2.27 <0.001 0.007 0.004 <0.5 23 50 48 2.19 <0.001 0.008 0.007 <0.5 22 43 53 2.23 <0.001 0.005 0.004 <0.5 17 45 33 2.20 <0.001 <0.005 0.003 <0.5 19 71 31 3.18 <0.001 0.005 0.003 <0.5 18 36 35 3.37 <0.001 0.006 0.004 <0.5 21 52 35 0.66 <0.001 <0.005 0.001 <0.5 27 36 25 3.15 <0.001 0.007 0.005 <0.5 22 83 43 3.38 <0.001 0.009 0.006 <0.5 14 47 22 3.06 <0.001 0.012 0.008 <0.5 17 91 29 3.16 0.001 0.007 0.005 <0.5 20 70 35 3.17 <0.001 0.007 0.006 <0.5 20 107 35 3.48 <0.001 0.006 0.005 <0.5 19 70 32 3.23 <0.001 0.010 0.007 <0.5 19 42 37 3.41 <0.001 0.008 0.006 <0.5 18 43 38 3.20 <0.001 <0.005 0.003 <0.5 18 91 36 0.06 0.042 0.174 0.341 <0.5 125 1300 1920 3.38 <0.001 0.005 0.005 <0.5 20 146 40 3.29 <0.001 0.006 0.003 <0.5 17 62 42 3.22 <0.001 0.007 0.005 <0.5 20 102 41 3.22 <0.001 0.007 0.006 <0.5 17 51 31 3.41 <0.001 0.006 0.005 <0.5 16 49 30 3.18 <0.001 0.020 0.013 <0.5 16 89 31 3.11 <0.001 0.006 0.004 <0.5 18 6 27

3.68 0.001 0.021 0.016 <0.5 19 102 43 2.08 0.001 0.028 0.025 <0.5 21 109 56 <0.02 0.001 0.031 0.025 <0.5 21 114 58 2.30 0.004 0.113 0.101 <0.5 28 128 153 1.94 0.001 0.036 0.034 <0.5 26 122 50 2.56 0.001 <0.005 0.001 <0.5 36 35 10 2.23 0.002 <0.005 <0.001 <0.5 45 105 33 2.25 0.001 <0.005 <0.001 <0.5 49 29 31 3.54 0.001 0.007 0.002 <0.5 39 165 33 3.43 <0.001 <0.005 0.001 <0.5 38 153 27 3.56 <0.001 <0.005 <0.001 <0.5 36 81 12 3.62 <0.001 <0.005 <0.001 <0.5 38 105 13 0.06 0.036 0.182 0.345 <0.5 122 1245 1925 3.73 0.004 0.017 0.003 <0.5 45 267 49 3.68 0.006 0.027 0.006 <0.5 47 256 65 3.27 0.004 0.016 0.003 <0.5 43 314 52 3.53 0.003 0.020 0.007 <0.5 44 263 55 3.70 0.003 0.022 0.010 <0.5 48 246 63 2.13 0.006 0.029 0.015 <0.5 44 160 72 2.31 0.004 0.029 0.018 <0.5 42 209 67 2.24 0.006 0.025 0.010 <0.5 50 248 80 2.42 0.003 0.022 0.014 <0.5 58 257 93 0.67 <0.001 <0.005 <0.001 <0.5 26 15 25 2.59 0.001 0.019 0.006 <0.5 63 124 194 2.57 0.005 0.029 0.018 <0.5 67 161 225 2.32 0.002 0.017 0.009 <0.5 68 142 235 2.48 0.002 0.018 0.007 <0.5 72 148 244 2.29 0.002 0.025 0.010 <0.5 73 140 259 2.53 0.002 0.024 0.013 <0.5 72 149 273 2.97 0.001 0.014 0.004 <0.5 69 142 273 2.58 0.001 0.021 0.008 <0.5 70 121 274 2.55 0.005 0.050 0.029 <0.5 70 163 286 0.06 0.175 1.825 0.850 <0.5 95 828 1790 2.51 0.004 0.032 0.020 <0.5 71 216 289 2.63 0.001 0.024 0.012 <0.5 69 230 250 2.20 0.002 0.036 0.022 <0.5 66 181 219 1.90 0.006 0.084 0.057 <0.5 73 223 371 1.73 0.011 0.083 0.056 <0.5 70 695 331 2.01 0.001 0.044 0.021 <0.5 69 166 250 2.34 0.014 0.178 0.127 <0.5 90 1310 410

2.49 0.003 0.026 0.013 <0.5 73 377 231 2.52 0.004 0.042 0.029 <0.5 72 355 221 <0.02 0.004 0.045 0.033 <0.5 67 336 212 2.38 0.002 0.030 0.020 <0.5 65 222 187 2.32 0.002 0.027 0.014 <0.5 63 167 186 2.35 0.017 0.049 0.029 <0.5 62 212 199 2.41 0.009 0.063 0.025 <0.5 64 380 219 2.43 0.006 0.040 0.022 <0.5 64 375 175 2.30 0.004 0.024 0.026 <0.5 64 263 142 1.77 0.004 0.055 0.049 <0.5 62 431 242 0.61 0.012 0.098 0.057 <0.5 73 191 372 1.28 0.001 0.058 0.030 <0.5 57 263 216 0.06 0.181 1.930 0.870 <0.5 96 830 1855 1.88 <0.001 <0.005 <0.001 <0.5 2 4 3 1.94 <0.001 <0.005 <0.001 <0.5 1 2 1 1.98 <0.001 <0.005 <0.001 <0.5 1 3 3 1.74 <0.001 <0.005 <0.001 <0.5 <1 2 2

3.34 0.016 0.117 0.011 <0.5 40 163 104 3.61 0.013 0.254 0.094 <0.5 46 131 142 3.51 0.018 0.290 0.150 <0.5 53 166 182 3.90 0.002 0.082 0.096 <0.5 56 77 174 3.69 0.002 0.027 0.045 <0.5 59 113 178 3.68 0.003 0.018 0.044 <0.5 57 134 171 0.06 0.039 0.182 0.346 <0.5 121 1200 1785 3.71 0.002 0.019 0.023 <0.5 67 110 239 3.82 0.001 0.015 0.008 <0.5 78 99 290 3.91 0.004 0.018 0.006 <0.5 75 77 273 3.72 0.002 0.018 0.013 <0.5 75 109 279 3.82 0.001 0.016 0.005 <0.5 78 61 289 3.60 0.002 0.028 0.009 <0.5 83 53 299 3.72 0.003 0.022 0.009 <0.5 86 69 317 3.67 0.002 0.034 0.012 <0.5 91 78 404 3.71 0.003 0.042 0.029 <0.5 102 135 535 0.72 0.001 <0.005 0.001 <0.5 25 30 25 3.52 0.002 0.035 0.017 <0.5 107 100 570 3.66 0.003 0.054 0.048 <0.5 111 105 603 3.38 0.007 0.053 0.038 <0.5 111 166 607 3.82 0.002 0.025 0.010 <0.5 111 100 578 3.26 0.004 0.045 0.029 <0.5 105 126 546 3.57 0.002 0.024 0.015 <0.5 101 91 513 4.05 0.002 0.036 0.026 <0.5 93 99 485 3.67 0.002 0.024 0.025 <0.5 96 113 474 3.54 0.001 0.021 0.014 <0.5 93 90 438 0.06 0.036 0.184 0.354 <0.5 128 1265 1890 3.74 0.002 0.013 0.006 <0.5 72 96 273 3.65 0.005 0.014 0.006 <0.5 70 110 232 3.46 0.002 0.020 0.005 <0.5 72 100 231 3.93 0.002 0.029 0.005 <0.5 69 86 208 3.83 0.002 0.020 0.005 <0.5 69 106 220 4.18 0.003 0.022 0.022 <0.5 62 95 219 3.97 0.002 0.023 0.007 <0.5 66 110 208 3.72 0.004 0.027 0.011 <0.5 67 132 204 3.89 0.002 0.022 0.019 <0.5 67 195 215 <0.02 0.003 0.026 0.031 <0.5 68 216 218 3.68 0.002 0.024 0.006 <0.5 66 116 191 2.63 0.002 0.019 0.003 <0.5 64 125 195 2.40 0.001 0.026 0.005 <0.5 68 103 188

2.48 0.023 0.014 0.005 <0.5 67 81 207 2.58 0.002 0.010 0.003 <0.5 67 55 214 2.46 0.001 0.013 0.006 <0.5 69 84 224 2.26 <0.001 0.007 0.004 <0.5 69 69 234 2.57 0.020 0.018 0.075 <0.5 73 206 268 1.66 0.009 0.068 0.113 <0.5 74 394 288 2.39 0.014 0.128 0.113 <0.5 126 680 683 2.21 0.080 1.190 0.730 0.7 130 1510 935 0.06 0.110 1.145 0.520 <0.5 91 804 1740 2.45 0.111 1.520 0.889 1.4 122 2500 1215 2.39 0.132 1.605 0.897 1.9 140 3130 1505 2.33 0.142 2.20 1.360 3.2 132 5190 1785 2.59 0.116 2.07 1.310 2.5 124 4730 1635 2.32 0.201 4.03 2.37 3.8 147 6480 2170 1.82 0.083 1.290 0.802 1.4 114 2380 1115 2.36 0.078 0.994 0.566 0.9 120 2080 1070 0.95 <0.001 0.007 0.004 <0.5 25 45 27 1.94 0.062 0.742 0.477 1.6 115 2300 1055 2.29 0.013 0.131 0.089 0.8 69 876 498 2.42 0.005 0.048 0.029 <0.5 68 582 444 2.24 0.042 0.635 0.364 0.9 103 1695 815 2.44 0.013 0.134 0.088 <0.5 83 796 563 2.61 0.072 1.130 0.699 1.7 128 3120 1240 2.45 0.086 1.290 0.797 2.6 149 4020 1555 2.59 0.034 0.481 0.287 1.0 122 1390 836 2.52 0.045 0.628 0.373 1.7 103 2200 879 0.07 0.182 1.920 0.883 <0.5 95 836 1805 2.49 0.056 0.827 0.512 1.9 124 2950 1095 2.37 0.013 0.141 0.094 0.7 88 878 509 2.43 0.009 0.056 0.033 0.7 74 767 482 1.24 0.019 0.277 0.169 0.8 98 870 513 2.28 0.004 0.040 0.024 <0.5 66 375 295 2.15 0.021 0.309 0.187 0.7 74 844 461 2.20 0.008 0.084 0.050 0.5 59 499 303 2.37 0.009 0.223 0.160 0.5 67 531 520 2.24 0.001 <0.005 0.007 <0.5 66 231 326 <0.02 0.001 0.005 0.007 <0.5 67 236 322 2.37 0.001 <0.005 0.005 <0.5 51 136 239 2.17 0.001 <0.005 0.004 <0.5 43 107 188 2.27 <0.001 <0.005 0.006 <0.5 53 177 246

2.45 0.008 0.086 0.056 0.6 44 516 218 2.43 0.002 0.038 0.030 <0.5 40 179 184 2.34 <0.001 <0.005 0.004 <0.5 36 91 163 2.18 <0.001 <0.005 0.002 <0.5 29 46 104 2.05 <0.001 <0.005 0.002 <0.5 34 7 81 0.06 0.171 1.890 0.882 0.5 88 792 1690